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    Characteristics, Genesis and Evolution of Daigu Landform in Yimengshan UNESCO Global Geopark
    CAI Yinlu, WU Fadong, HAN Jinfang, HUANG Zhen, ZHOU Ying, LIU Baoyin, CHEN Yangyang
    Geoscience    2023, 37 (04): 1065-1074.   DOI: 10.19657/j.geoscience.1000-8527.2023.085
    Abstract1857)   HTML14)    PDF(pc) (12188KB)(507)       Save

    The Yimengshan UNESCO Global Geopark (UGGp) is the origin of the “Daigu Landform”. Through field investigation of the characteristics of Gu landform, based on the measurement of river valley stratigraphy and profiles, and using the OSL dating of the river terrace to calculate the cutting rate, the formation time of Daigu Landform has been determined. The results show that the geomorphological features of the Daigu Landform are related to the strata lithology of the Gu body. Daigu Landform is a type of mesa structure, with a flat top, steep margin and gentle slope. Gu body is mainly composed of two strata with different lithologies: The top comprises Cambrian limestone with strong weathering resistance but develops many joints, while the Gu body with weak erosion resistance is dominated by mudstone and siltstone. We estimated that the formation time is about 1.77 Ma by using the erosion rate, based on the dating results of the river terrace. The Daigu Landform formation and evolution can be divided into four main stages: (1) the material was formed in the Early Cambrian; (2) tectonic uplift, and the strata gradually exhumed and the shaping stage began; (3) long-term weathering and denudation of various external forces, such as surface water that gradually created the mature Daigu Landform; (4) the landform ended its development when the upper limestone collapsed. The systematic study of the Daigu Landform has great importance in understanding the Daigu Landform and its scientific value, which also contributes to the spreading of geoscience knowledge of UGGps.

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    Redox Sensitive Trace Element Compositions of the Shuinan Formation Black Shale in the Laiyang Sag: Controlling Factors of Organic Matter Enrichment
    WANG Xuxue, ZHANG Xiangyu, LI Shoujun, ZHANG Jiahao, ZHANG Zhenyu
    Geoscience    2023, 37 (03): 733-744.   DOI: 10.19657/j.geoscience.1000-8527.2021.153
    Abstract430)   HTML3)    PDF(pc) (7945KB)(164)       Save

    The geochemical characteristics of mudstone and shale in the saline lake basin are of great significance to the formation conditions and sedimentary environment of saline Source rock. To reconstruct the redox conditions and explore the controlling factors of organic matter enrichment in the Lower Cretaceous Laiyang Group of the Laiyang Sag, redox sensitive elements (RSEs, such as Mo, Cr, Zn, Cu, Ni, Co, V, As, U and Th) and total organic carbon (TOC) of mudstone and shale from this Group were analyzed. The results show that TOC content of mudstone in the Wawukuang and Zhifengzhuang Formations is relatively low, and that RSEs are not obviously enriched. TOC content of Shuinan Formation black shale increases sharply, and RSEs are enriched significantly, suggesting a weakly reducing environment. TOC content of the Longwangzhuang and Qugezhuang Formations decreases rapidly, and the RSE content is low, suggesting an oxidizing environment. Organic matter enrichment in the Shuinan Formation black shale is likely related to a combination of paleoclimate, paleoproductivity, paleosalinity and redox factors, among which paleoclimate is the main controlling factor of paleoproductivity, paleosalinity and redox conditions.

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    Advances on the Understanding in the Emeishan Mantle Plume and Dynamic Mechanism of the Permian Sichuan Basin Formation
    SUN Ziming, BIAN Changrong, LIU Guangxiang
    Geoscience    2023, 37 (05): 1089-1099.   DOI: 10.19657/j.geoscience.1000-8527.2023.043
    Abstract380)   HTML19)    PDF(pc) (4559KB)(320)       Save

    In recent years, significant research progress has been made on the Emeishan Large Igneous Province (ELIP) and its genetic mechanism of mantle plume, but the scope of the mantle plume on the Sichuan Basin and the dynamic mechanism for the Permian sedimentary basin formation remain unclear.Based on a number of literature research and recent studies, and the idea that deep mantle activity controls the evolution of crustal surface system, the characteristics of Emeishan LIP and its deep geology are systematically reviewed.It is recognized that the mantle plume is the dominant factor that induces the large-scale eruption of the Emeishan basalts and formed the LIP, and has direct influence on some parts of the Sichuan Basin, which is manifested by the differential denudation of the top Middle Permian Maokou Formation.This was likely caused by the upwelling of mantle plume and its control on the Permian sedimentation and sedimentary facies distribution in the central-southern part of the basin.Formation of the extensional troughs, and the alternating high-and-low sedimentary-tectonic framework in the central-northern Sichuan Basin during the Permian to Early Triassic may have been mainly controlled by the extension of the southern Qinling Ocean.

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    Strontium in Soil-crop Migration and Enrichment Discussion on the Standard of Strontium Enrichment in Crops:A Case Study from the Shihe Area in Gushi, Henan
    WANG Dongxiao, YUAN Dezhi
    Geoscience    2023, 37 (03): 767-777.   DOI: 10.19657/j.geoscience.1000-8527.2023.024
    Abstract282)   HTML14)    PDF(pc) (4917KB)(298)       Save

    By systematically collecting and analyzing soil and crop samples in the Shihe river basin of Gushi (Henan Province), and conducting geochemical evaluation of land quality, we identified regional soil Sr geochemical characteristics, influencing factors, and migration and enrichment mechanisms in soil and crops, i.e., residue state>strongly organic bound state>ion-exchange state>ferromanganese oxidation state>humic acid bound state>carbonate bound state>water-soluble state account for 98%. Strontium exists primarily in the soil in an insoluble stable form. In a weakly acidic environment, the insoluble Sr-bearing minerals (SrSO4 and SrCO3) hydrate and hydrolyze to form water-soluble Sr(HCO3)2 and SrCl2, which are absorbed and utilized by plants to facilitate Sr migration in soil and crops. The Sr-rich standard for peanut, wheat, corn, rice, and other crops was proposed by comparing the Sr content of related crops (domestic and international), i.e., the lower limit is 0.65 mg/kg for Sr-rich rice, and 1.08 mg/kg for Sr-rich peanut, wheat, and corn. According to this Sr content standard, our wheat and peanut (and some rice) samples are Sr-rich. Our results provide a new reference for the development of Sr-rich land resource and Sr-rich agricultural products in the Shihe river basin.

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    Record of Mesozoic Collision Orogeny on the Eastern Section of the West Kunlun Orogen: Evidence from Geochronology and Geochemistry of the Triassic Wenquan-Shenglidaban Granitic Intrusions, Xinjiang
    LU Hao, LIU Huan, HU Feng, WANG Haibo, WANG Chao, KONG Xiangchao
    Geoscience    2023, 37 (03): 573-585.   DOI: 10.19657/j.geoscience.1000-8527.2022.022
    Abstract273)   HTML7)    PDF(pc) (6485KB)(595)       Save

    Many Triassic intrusive rocks are emplaced in Wenquan-Shenglidaban area in the eastern section of the West Kunlun orogen. The lithology mainly includes medium-/fine-grained monzogranite, which records the Mesozoic tectonic evolution of the orogen and provides chronological constraints for the metallogenic age of gold, mercury, antimony and other metals in this area. In this study, detailed analyses on the petrology, whole-rock chemistry and zircon U-Pb geochronology of the Lower Triassic Adamupa lower series granites are presented. The results show that the Wenquan-Shenglidaban granite was emplaced at (203.3±1.4) Ma, indicating a product of the Late Triassic magmatic activity. The rocks have SiO2, Na2O, K2O and A/CNK of 74.41%-76.78%, 2.70%-3.81%, 3.93%-5.01% and 1.00-1.25, respectively, indicating that the granites are peraluminous high-K calc-alkaline with low total rare earth element contents. The granites are rich in light rare earth elements and negative Eu anomaly (δEu=0.39), and are relatively rich in Rb, Th and U, but depleted in Ba, Nb, Sr, and Ti. This indicates that the granites are crustal-derived S-type. Combined with the regional tectonic evolution, the Atamupa granite was likely formed in the post-orogenic stage. It is probably a post-collisional granite sourced by the partial melting of the subducted metamorphic clastic rocks into the lower crust. The resulted magma then ascended and emplaced at upper crust and the granites was formed.

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    Geochronology and Tectonic Setting of the Lamasu Cu Deposit in Northern Xinjiang: Evidence from In-situ LA-ICP-MS Garnet U-Pb Dating
    WANG Xiaotong, LIU Jun, YANG Yan, HE Juncheng
    Geoscience    2023, 37 (03): 645-661.   DOI: 10.19657/j.geoscience.1000-8527.2023.003
    Abstract259)   HTML7)    PDF(pc) (10155KB)(165)       Save

    Garnet, as a typical altered mineral in skarn deposits, is suggested to be an important mineral for obtaining accurate ore-forming age. There are abundant skarn Cu deposits in the Chinese Western Tianshan, yet the actual skarn Cu ore-forming ages remain controversial. This limits sufficient understanding of skarn Cu ore genesis and metallogenic dynamic background in the Chinese Western Tianshan. To obtain accurate metallogenic age of skarn Cu deposits in the Chinese Western Tianshan, we selected garnet from the Lamasu Cu deposit for systematic geochemical and geochronological study by Electron Probe X-ray Micro-Analyzer (EPMA) and LA-ICP-MS U-Pb dating. According to the hand-specimen and petrographic characteristics of the garnet minerals, the Lamasu deposit has three types of garnets, including red-brown, light-brown and yellow-green garnets. These garnets belong to the andradite-grossularite series, and occur as andradite (56.96%-85.09%) with minor grossularite (14.33%-43.85%). Three types of garnets yielded LA-ICP-MS U-Pb weighted average ages of (389.1±2.0) to (387.0±2.3) Ma, indicating that the Lamasu Cu mineralization occurred during the Middle Devonian subduction of the northern Tianshan oceanic crust.

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    Geochemical Genes for the Weathering of Dolomite at the Shangmanggang Gold Deposit Area in Luxi, Yunnan, SW China
    ZHANG Gaixia, SUN Jinjiajie, GONG Qingjie, JIANG Biao, YAN Taotao
    Geoscience    2023, 37 (03): 801-812.   DOI: 10.19657/j.geoscience.1000-8527.2022.087
    Abstract252)   HTML11)    PDF(pc) (2408KB)(117)       Save

    Geochemical gene is a new technique to classify and trace geological materials. The current research focuses on testing the gene steady properties and traceability of soils from the weathering of magmatic and (minor) carbonate rocks. Two weathering profiles developed on dolomite in the Shangmanggang gold deposit at Luxi (Yunnan Province, SW China) were investigated for the steady properties of geochemical genes, including lithogenes (LG01 and LG03), metallogene (MGAu and MGW), and REE (rare earth element) genes (REEG01 and REEG02). The geochemical results indicate that the dolomite was totally leached during the pedogenetic stage, followed by the soil evolution stage. Chemical weathering indices of CIA (chemical index of alteration) and WIG (weathering index of granite) were used to quantify the degrees of weathering, however the CIA may indicate the weathering degrees of the provenance sediments of dolomite. Therefore, WIG is better than CIA to determine the weathering degrees of carbonate rocks. Based on the results of heredities and inheritances of geochemical genes on weathering products, the parent rocks may have been geochemically homogeneous. The dolomite and its weathering products are classified as the intermediate-like compositions on felsic similarities of lithogenes, as anomalous gold-mineralized samples on mineralization similarities of gold metallogene, similar to the upper continental crust on REE genes. Although the anomaly materials classified on mineralization similarities of gold metallogene are not necessarily gold ores, they have likely the potential to offer ore-forming materials. The mineralization similarity of gold metallogene can be used to determine whether a weathering-type deposit was formed on the parent rock, which offers new insight or technique on tracing the provenance of ore-forming materials.

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    Deformation Characteristics and Revival Mechanism of Yahuokou Multi-stage Landslide in Zhouqu, Gansu Province
    YANG Xiaohui, ZHU Peng, YUAN Zhongxia, ZHANG Weixiong, DING Baoyan
    Geoscience    2023, 37 (04): 1004-1012.   DOI: 10.19657/j.geoscience.1000-8527.2021.157
    Abstract244)   HTML21)    PDF(pc) (10274KB)(116)       Save

    On July 19th, 2019, a multi-stage landslide (volume: 215.5×104 m3) with a reactivated sliding in the middle groove of the paleo-landslide occurred in Yahuokou (Zhouqu County,Gansu Province). The landslide started from the cliff mouth at the top of the slope body, and slowly slid down to the Minjiang River with flow shape. This blocked the Minjiang River channel and raised the water level, seriously threatening the safety of nearby residents and downstream towns. To study the deformation characteristics and revival mechanism of the landslide, the landslide geo-environmental background and deformation history were first investigated through field survey and historical data analysis. With data interpretation on remote sensing, landslide monitoring and rainfall, the landslide initiation and evolution processes were elucidated, and the landslide revival mechanism revealed. The multistage landslide resurrection is characterized by stepwise loading, stress transfer, and initiation. The landslide revival comprises three stages: (1) the upper slide began to flow slowly in a plastic form; (2) the middle platform of the gentle slope was prepressed by the upper sliding body, forming the “cut-fill” effect. Its failure mode is creep slip-tensile crack-sliding; (3) the lower block slid.

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    Characteristics of Stromatolites and Its Significance in Depositional Environment Reconstruction of the Mesoproterozoic Longjiayuan Formation (2nd Member), Western Henan
    LI Qianqian, ZHENG Deshun
    Geoscience    2023, 37 (04): 845-857.   DOI: 10.19657/j.geoscience.1000-8527.2022.023
    Abstract232)   HTML27)    PDF(pc) (12773KB)(573)       Save

    Stromatolites recorded the life activities of early environment, cyanobacteria and microbial community, and their growth morphology was influenced by the sedimentary environment, which is of great significance for the paleo-environmental reconstruction. Stromatolites from the Longjiayuan Formation (2nd member)of the Mesoproterozoic Guandaokou Group in western Henan have various morphological types and concentrated in distribution, which is a typical area for stromatolites development. The distribution of stromatolites is closely related to global events, geochemical environment of the Precambrian ocean and the development of microbiolites, yet detailed research is still lacking. Based on this, we conducted a systematic field investigation and petrological examination on the microbialite structure on these stromatolites, studied the macroscopic and microscopic characteristics of the stromatolites, established the sedimentary environment evolution and sedimentary model, and compared with the stromatolites from other areas. The results show that the macroscopic morphology of the stromatolites can be divided into horizontal laminae, ripple, hilly, cone, and column. Microscopically, the stromatolites are light and dark laminae, with few ooids, spherular and detrital materials locally. The shape and scale of stromatolites are closely related to the hydrodynamic conditions and water depth. Horizontal laminated stromatolites were developed in the intertidal zone, whilst corrugated and mound stromatolites were developed in the intertidal high-energy zone and low-energy zone. Meanwhile, cone and columnar stromatolites were developed in the subtidal zone. Our comprehensive analysis shows that our stromatolite samples were formed in a tidal-flat environment, and were influenced by the sedimentary evolution process of intertidal, subtidal and intertidal zones. It is beneficial to analyze the Early Mesoproterozoic development environment of microbiolites in the southern margin of North China. Besides, we compared our results with the sedimentary environment of microbiolites in Jixian area (northern margin of North China), in order to explore the relationship between marine environment, atmospheric environment, and microbiolites around the North China Craton.

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    Depositional Environment and Sedimentary Model of the Fengcheng Formation in Mahu sag, Junggar Basin
    NI Minjie, ZHU Hexuan, HE Wenjun, YANG Sen, ZOU Yang, ZHANG Yuanyuan
    Geoscience    2023, 37 (05): 1194-1207.   DOI: 10.19657/j.geoscience.1000-8527.2023.061
    Abstract226)   HTML12)    PDF(pc) (31168KB)(211)       Save

    The Mahu sag is one of the most prolific oil-gas sags in the Junggar Basin.The Lower Permian Fengcheng Formation is the main high-quality lacustrine source rocks, and is considered as the key exploration target in the Mahu sag.The lithofacies distribution and sedimentary environment of the Fengcheng Formation are of great significance in studying the tectonic evolution and further oil-gas exploration of the Mahu sag.Based on the latest logging data, we established a comprehensive stratigraphic column for the Fengcheng Formation from well Maye 1, and clarified the lithofacies distribution of the Fengcheng Formation.The tectonic sedimentary environment and sedimentary model of the Fengcheng Formation are constructed subsequently.The Fengcheng Formation is mainly composed of dark fine-grained sedimentary rocks in well Maye 1, with a large number of soft-sediment deformation structures.The middle member of the Fengcheng Formation was likely deposited in (semi-)deep lacustrine facies.According to the lithofacies profile in the Fengcheng Formation, the cyclic characteristics of progradation-retrogradation-progradation developed from bottom to top, and the sedimentary facies changed from fan delta, lacustrine to river delta facies from southwest to northeast.Volcanism likely played a key role in the lower member of the Fengcheng Formation of shallow lacustrine facies in the northern part of Mahu sag.In the middle member of the Fengcheng Formation, the southern part of Mahu sag developed fan-delta deposits, which is transformed into delta-shore shallow lacustrine deposit to the west of Mahu sag, and semi-deep to deep lacustrine deposits are developed in the northern part.The middle member of (semi-)deep lacustrine facies is characterized with extensive distribution and abundant alkaline minerals in the depocenter.The chemical precipitation in the middle member of the Fengcheng Formation is the most widely distributed, indicating the maximum flooding surface.The progradation in the upper member of the Fengcheng Formation may have resulted from shrinking of the sag.Fan delta deposits are developed in the southern and western parts of the Mahu sag, and semi-deep lacustrine to shore-shallow lacustrine facies are developed in the northern part.Combined with its sedimentary evolution process, the Fengcheng Formation is likely deposited and multiple-sourced, including terrigenous clastic deposits, endogenous chemical precipitates and pyroclastic material.

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    Sedimentary Characteristics of Late Quaternary Loess in Hexigten Global Geopark and Its Paleoclimatic Implications
    LIU Xiaohong
    Geoscience    2023, 37 (03): 821-833.   DOI: 10.19657/j.geoscience.1000-8527.2023.071
    Abstract223)   HTML17)    PDF(pc) (12425KB)(420)       Save

    Loess has various paleoclimatic indicators, among which the particle size and magnetic susceptibility are important objects for paleoclimate research, and detailed studies on loess layers in different regions can faci-litate global climate change comparison and climate cycle division. Taking the Holocene Sanyixiang loess profile and the Upper Pleistocene Tuchengzi loess profile of Hexigten Global Geopark as an example, the loess samples were subjected to 14C dating, photoluminescence dating, grain size and magnetic susceptibility analyses. The regional paleoenvironmental change since the Late Quaternary was reconstructed, which provided a new and strong evidence for studying the climate types in northern China. The 14C dating on the Sanyixiang profile yielded 2.32 ka, 9.05 ka, 9.94 ka and 11.27 ka, whilst the OSL dating on the Tuchengzi profile yielded 21.5 ka, 23.5 ka, 43.9 ka, 53.4 ka, which show that the Sanyixiang and Tuchengzi profiles are Late Quaternary. The Sanyixiang and Tuchengzi profiles are young and old, respectively, forming a relatively complete loess sequence. The study shows that coarse silt(16-63 μm) was a major course-size component in the loess-paleosol deposition, accounting for 61.45%-62.4%, followed by sand(>63 μm) and clay(<4 μm). Based on stratigraphic features and grain-size curve, the Hexigten area underwent cold-hot, dry-humid cycles and at least four summer monsoon intensifying events. The grain size and magnetic susceptibility records of the Sanyi-xiang/Tuchengzi loess profiles are basically similar to those of the Luochuan profile of the loess plateau, with coarser grain size and lower magnetic susceptibility during the glacial period. Meanwhile, the magnetic susceptibility of the interglacial or interglacial step increases significantly, and the grain size becomes significantly smaller, indicating that the paleoenvironmental evolution of the two places was controlled by the East Asian monsoon intensity in a glacial-interglacial timescale.

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    Research Progress and Prospect of Groundwater Pump and Treat Technology
    ZHANG Li, LIU Fei, YUAN Huiqing, LIANG Kaixuan
    Geoscience    2023, 37 (04): 977-985.   DOI: 10.19657/j.geoscience.1000-8527.2022.030
    Abstract220)   HTML9)    PDF(pc) (5730KB)(300)       Save

    Groundwater pump and treat technology (P&T) is a representative technology of groundwater reme-diation, and is at present widely used also to control and repair groundwater pollution. However, in the practical application of P&T technology, it is often interfered by the complexity of hydrogeological conditions and the special behavior of ground pollutant migration and transformation. The most important problem is tailing or rebound, which leads to low efficiency and high cost in the later stage of treatment. Based on expounding the development and evolution of P&T technology, we systematically analyzed its application conditions, technological pros and cons, system design optimization methods and its combined use with other technologies. We concluded that with the application of pumping treatment, it is more used for the pump of high concentration pollutants in the initial stage of pollution and hydraulic control to avoid pollutant diffusion. Currently, the goal of pumping changes from treatment to flow field control. The pumping/injecting wells are often located at the contamination source and plume and their upstream and downstream. The purposes of controlling pollutant diffusion and clean water diversion were achieved by pumping the contaminated water or injecting uncontaminated water into the ground to form a watershed. Our results provide suggestions for the flexible application of groundwater pump technology and the selection of prevention and control solutions for site groundwater pollution in China.

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    New Perspectives of the Features, Formation, and Evolution of the Special Danxia Landscape in Chenzhou, Hunan
    HUANG Leqing, WU Chihua, ZHOU Liyun, JIN Ni, PENG Shiliang, HU Nengyong, YANG Changming, CHEN Jie
    Geoscience    2023, 37 (06): 1680-1694.   DOI: 10.19657/j.geoscience.1000-8527.2023.118
    Abstract218)   HTML19)    PDF(pc) (21126KB)(460)       Save

    The Feitianshan-Gaoyiling area in Chenzhou (Hunan Province) is a prominent attraction in South China, known for its distinctive Danxia landform. Unlike typical Danxia landscapes, this area features distinct dome mounds. However, despite its social popularity and scientific value of its unique geomorphology, detailed studies on its geomorphological features, internal genetic mechanism, and evolution have long been overlooked. Through field investigations, we discovered that the Danxia landform in the Feitianshan-Gaoyiling area has seven geomorphological subtypes, including stone village, rock mound, Chibi, stone column, stone wall, cave, and linear trench. Notably, the eastern and western sides of the study area display distinct differences in the Danxia landscape. The eastern side is dominated by dome mounds and stone villages, where the structural strata comprise of eolian desert-facies sandstone, characterized by significant eolian sedimentary structures such as giant staggered bedding, small-scale granular flow layers, and corrugated layers. Meanwhile, the western side of the area features a “top slope, steep slope, foot gentle” peak forest-type Danxia landscape, primarily composed of alluvial fan massive conglomerates. The variations in lithofacies types between the eastern and western sides are the main factors contributing to the diverse geomorphological forms, developed through multistage tectonic transformation, water erosion, weathering, and collapse in the Himalayan period. Using the analysis of the area elevation integral model (HI), we determined that the local Danxia landform is in the early residual hill stage of old age. Accordingly, we propose a three-stage landscape model of “sedimentation pregnant landscape-tectonic uplift landscaping-surface force carving landscape”, to analyze the Danxia landform origin and enhance the brand connotation of Danxia scenic landforms. We aim to better understanding in the distinctive landscape of rock-like Danxia in the humid South China climatic region, and to provide scientific guidance and reference for the development and utilization of Cretaceous Danxia landform geological heritage in South China.

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    Study on Seepage Mechanism Characteristics of A Single Fracture Based on Fracture Deformation Under Different Confining Pressures
    CHENG Zhiyu, LIU Rui, ZHANG Jinfeng, MA Haichun, WANG Jingping
    Geoscience    2023, 37 (04): 972-976.   DOI: 10.19657/j.geoscience.1000-8527.2023.059
    Abstract217)   HTML5)    PDF(pc) (1538KB)(173)       Save

    It is necessary to study the seepage flow under different confining pressures in laboratory because the real groundwater flow and solute transport are affected by the extensive and complex distribution of in-situ stress. In practical projects such as groundwater pollution prevention and control, the permeability of fractures is signi-ficantly affected by confining pressure. Based on the basic constitutive law, the seepage flow under confining pressure is analyzed quantitatively in this paper. Based on the deformation of hydraulic aperture and the defor-mation law of fracture, the relationship model between seepage characteristics (seepage pressure Ps, hydraulic aperture eh and permeability k) and confining pressure Pc under confining pressure is established. The hydraulic experiment of a single fracture of marble is carried out in a core holder, and the experimental data are regressed. It is verified that the model has a high fitting effect. It can effectively predict the relationship between the seepage characteristics (seepage pressure, hydraulic opening and permeability) and the surrounding pressure.

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    Source Analysis and Spatial Distribution of Heavy Metals in Soil from Typical Open-pit Coal Mines in the Gobi Desert, Xinjiang
    DUGUER Weiwei, SHI Haitao, XING Hao, LOU Xuecong, HU Hongli, BULONG Bate
    Geoscience    2023, 37 (03): 790-800.   DOI: 10.19657/j.geoscience.1000-8527.2023.041
    Abstract216)   HTML4)    PDF(pc) (6091KB)(218)       Save

    Identifying the sources and spatial distribution characteristics of heavy metals in soil of typical opencast coal mines in Gobi desert is crucial in accurately judging and formulating soil pollution control programs. However, systematic research is still weak inadequate. In this study, 266 soil samples were systematically collected around typical coal mines in the Xinjiang Gobi Desert. Soil As, Cd, Co, Cu, Cr, Hg, Ni, Pb, Zn contents and pH values were measured. By using descriptive statistical, correlation, cluster and principal component analyses and other multivariate geostatistical analysis methods,the soil heavy metal compositions were analyzed and the heavy metal source preliminarily identified. We used the absolute principal components-multiple linear regression receptor model(APCS-MLR) and inverse distance weighting method to quantify the contribution rate of each pollution source and the heavy metal spatial distribution patterns. The results show that:(1) The average soil pH is 8.31 in the study area, the contents of nine elements were lower than the threshold for agricultural and construction land, and also below the soil heavy metal background in Xinjiang. From the functional partitions, only the As, Cd, Cu, Ni and Pb contents in the waste sewage discharge area are higher than the Xinjiang background; Cr,Ni, Zn, Co, Cu, As and Cd have moderate or high correlations, Cd and Pb have moderate correlations, and Hg has weak correlations with the other eight elements. (2)Cr, Ni, Zn, Co, Cu, As and Cd have moderate or high correlations, Cd and Pb have moderate correlations, and Hg has weak correlations with the other eight elements.(3)The cluster analysis results divide the soil heavy metals into three categories: Cr-Ni-Zn-Co-Cu-As, Cd-Pb, and Hg. (4) Source analysis results show that the main heavy metal sources of local soil are parent material (50.902%), waste water and coal dust (31.507%).

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    Characteristics of Structural Superimposed Halo and Deep Prospecting Prediction of Yongxin Gold Deposit, Duobaoshan Area,Heilongjiang Province
    LI Chenglu, FU Anzong, XU Wenxi, YUAN Maowen, LIU Baoshan, YANG Wenpeng, ZHAO Ruijun, ZHAO Zhonghai
    Geoscience    2023, 37 (03): 674-689.   DOI: 10.19657/j.geoscience.1000-8527.2023.012
    Abstract216)   HTML18)    PDF(pc) (8511KB)(338)       Save

    The Yongxin gold deposit is one of the major prospecting achievements in recent years in the periphery of the Duobaoshan ore concentration area in Heilongjiang Province. It is the first discovered large-scale epithermal-type gold deposit related to the Nenjiang-Heihe mélange belt. The orebody has dip angle of 20°-30°, strictly controlled by structures, and extends over 400-meter long and nearly 1,600-meter deep. Deep exploration shows that the orebody is obviously thinner and the grade is lower. To further clarify the mineralization potential at depth and guide future exploration, the tectonic superimposed halo samples were taken in different exploration lines of the mining area for geochemical analyses. The geochemical statistical analysis shows that the element assemblage at Yongxin comprises Au, Ag, Pb, Mo, W, Bi, Mn and Te, among which Au is the most direct and important indicator for the formation of gold orebodies and Ag-Te is an important associated element. Based on the axial distribution characteristics of the inner, middle, and outer zone anomalies of each indicator element in the orebody, the axial zoning sequence of orebody halo at Yongxin is established: Sb-As-Hg → Ag-Au-Te-Pb-Zn-Cu → (Bi)-Mo-Mn-Co. Among them, Sb-As-Hg are the frontal halo indicator elements, Ag-Au-Te-Pb-Zn-Cu are the near-ore indicator elements, Mo-Mn-Co are the terminal halo indicator elements. The orebody axial characteristics show that the frontal-terminal halo coexists in the margin of orebody, indicating possible existence of orebody in deep structures. According to the prediction mark of tectonic superimposed halo and geological mark, a concealed ore prediction target and a favorable ore-forming site are proposed on the horizontal projection map. The targets are located between No. 205 and 225 exploration lines, whilst the favorable ore-forming sites are located between No. 235 and 245 exploration lines. Both show the coexistence of frontal and terminal halo in the middle and lower parts of the orebody, and the anomalies of frontal and near-ore elements are obviously stronger than those of the terminal halo elements. This indicates that the orebody extends downward significantly, which shows that it is worthy of further deep exploration.

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    Regional Geochemical Data Analysis Using Isometric Log-ratio Transformation and Mixture Distribution
    LI Zhu, ZHANG Dehui, YANG Fan, LIU Xiangchong
    Geoscience    2023, 37 (03): 662-673.   DOI: 10.19657/j.geoscience.1000-8527.2023.009
    Abstract205)   HTML21)    PDF(pc) (12589KB)(298)       Save

    Regional geochemical exploration data are typical compositional data. Isometric log-ratio transformation (ILR) produces an orthonormal basis of geochemical data, which can eliminate the data closure effect and account for the data compositional nature. However, it is still difficult to interpret ILR-transformed variables. To make ILR transformations easier to understand, geological knowledge and data-driven methods are used to construct the interpretable ILR-transformed variables. This method was applied to extract geo-information from stream sediment geochemical data in the central and southern Da Hinggan Mountains, Inner Mongolia, northern China. Based on these geological information and hierarchical cluster analysis, sequential binary partition was constructed among the Sn, W, Cr, and Ni concentrations, and expressed as variables b1, b2 and b3 by ILR transformation. Furthermore, the expectation-maximization (EM) algorithm modified by a minimum message length criterion (MML) was employed to investigate the variables mixture distributions.The ILR-transformed variables follow either a bi-normal or tri-normal distribution, which were interpreted as fingerprints inherited from mafic magmatic, Sn-W hydrothermal, and later geological processes. The high-average subpopulation of b1, b2 and b3 variables of ILR transformation corresponds to the anomalies of W-Sn metallogenic system, and four areas were predicted to have high Sn-W prospecting potential. This study shows that the ILR transformation and MML-EM algorithm are promising tools to effectively extract geo-information from geochemical data and delineate anomalies.

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    Genetic Mechanism of the “Yucheng-Type” High-Grade Skarn Iron Deposits
    ZHANG Zhaochong, WANG Huaihong, XIE Qiuhong, SHEN Lijun, ZHU Yuzhen, LÜ Yunhe, JIN Bowen
    Geoscience    2024, 38 (01): 1-12.   DOI: 10.19657/j.geoscience.1000-8527.2024.003
    Abstract198)   HTML49)    PDF(pc) (16652KB)(427)       Save

    The discovery of high-grade skarn iron deposits in the Qihe-Yucheng area of northwestern Shandong Province is a significant breakthrough for iron prospecting in China.It is expected to become another potential important base of high-grade iron ore resource in Shandong Province after Laiwu, Jinling, and Jinan areas.Unlike traditional skarn iron deposits hosted in the contact zone between intrusions and carbonate rocks, the Litun iron orebodies in the Qihe-Yucheng area are hosted in the Carboniferous-Permian coal-bearing strata.The high-grade iron orebodies have a sharp contact with the surrounding rocks, which have been changed to horns in a large range.We attribute the occurrence of the iron orebodies in the Carboniferous-Permian coal-bearing strata far from the contact zone to the extremely low thermal conductivity of the overlying coal rocks, which allow the hydrothermal fluid to maintain a high-temperature state and long-distance migration.The formation of the Litun iron deposit may be ascribed to the rapid precipitation of magnetite due to decreasing temperature and salinity caused by the mixing of high-temperature magmatic fluid and low-temperature meteoric water.In addition, strong albitization commonly occurs near ore bodies, leading to the loss of iron in the dioritic rocks, which lays an important material foundation for the exsolution of iron-rich fluids and the formation of high-grade iron ores.Finally, we propose that the mantle-derived “highly differentiated” diorite and hypabyssal emplacement is favor for the exsolution of magmatic fluids, and is also prerequisites for the formation of the Hanxing-type iron deposit.

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    Characteristics of the Hydrocarbon Accumulation Formed Through the Three Structural Cycles in Tarim Basin
    YANG Xianzhang, NENG Yuan, XU Zhenping, LI Kuayue, HUANG Shaoying, DUAN Yunjiang
    Geoscience    2024, 38 (02): 287-299.   DOI: 10.19657/j.geoscience.1000-8527.2023.078
    Abstract173)   HTML18)    PDF(pc) (16006KB)(253)       Save

    The Tarim Basin was formed through three major extensional-compressional tectonic cycles: Nanhua-Middle Devonian, Late Devonian-Triassic, and Jurassic-Quaternary. This multi-cycle tectonic evolution led to the complexity of the oil and gas accumulation and distribution. In recent years, the ultra-deep layer of the basin has become the key exploration area of oilfield. It is necessary to investigate the hydrocarbon accumulation law of the basin. According to the latest seismic data, drilling data, and oil and gas geological data, we find that the main source rocks of oil and gas accumulation in Tarim Basin are Triassic-Jurassic in the Kuqa area, and the Carboniferous-Permian continental source rocks in southwestern Tarim Basin, the Cambrian marine source rocks in the platform basin area. The development of the source rocks and reservoir-seal assemblages in the basin is controlled by the three major extensional-compressional tectonic cycles of the basin. The development position of the source rocks determines the development of the four petroleum systems in Tarim Basin, including the Kuqa piedmont, northern depression, Maigaiti slope, and southwestern Tarim piedmont. The basin has undergone the three major extensional-compressional cycles, and the hydrocarbon accumulation assemblages in the platform basin area, Kuqa foreland and southwestern Tarim foreland are distinct. The Carboniferous gypsum mudstone and Silurian-Carboniferous marine sandstone, Ordovician mudstone, and limestone, Middle Cambrian gypsum salt rock, and Sinian-Cambrian dolomite reservoir-cap assemblages occur in the basin. The Neogene-Quaternary mudstone and sandstone, Paleogene gypsum salt layer, Cretaceous sandstone reservoir, Jurassic mudstone, and Triassic-Jurassic sandstone reservoir-cap assemblage occur in the Kuqa area. The Miocene mudstone-sandstone, Paleogene gypsum-salt layer, and Cretaceous sandstone, Carboniferous-Permian mudstone and carbonate reservoir-cap assemblages are developed in the southwestern Tarim Basin, which constitute the upper, middle, and lower assemblages of the platform basin, Kuqa and southwestern Tarim Basin, respectively. The hydrocarbon expulsion of the source rocks in the basin occurred in late Caledonian, late Hercynian-Indosinian and Himalayan, forming three stages of oil and gas filling. Combined with the development characteristics of lithology, fracture, unconformity, and uplift in the key transformation period of Tarim Basin, the three-stage accumulation model of the basin is proposed.

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    Deep Reservoir Characteristics and Control of Physical Properties of Qigu Formation in the Western Section of the Southern Margin of Junggar Basin
    DENG Yi, GAO Chonglong, WANG Jian, LIU Ming, MENG Yuanlin, REN Ying, LIU Ke, WANG Ke
    Geoscience    2024, 38 (02): 335-349.   DOI: 10.19657/j.geoscience.1000-8527.2023.069
    Abstract172)   HTML11)    PDF(pc) (19321KB)(137)       Save

    The deep clastic reservoir of Qigu Formation in the western section of the southern margin of Junggar Basin has a great potential for oil and gas exploration. However, there is still a lack of systematic studies on its reservoir characteristics and control of physical properties, which seriously restricts the subsequent oil and gas exploration. With the combination of the relevant studies of regional burial history and paleogeothermal temperature, this paper comprehensively utilized the data of casting thin sections, scanning electron microscopy, physical properties, mercury intrusion and inclusions, and systematically studied the petrological characteristics, physical properties, diagenesis characteristics, and physical property control of the Qigu Formation reservoir. The results show that the Qigu Formation reservoir exhibits the petrological characteristics of low compositional maturity, high plastic debris content, and medium structural maturity. Although the buried depth of the reservoir center is more than 3,500 m, the reservoir space is still dominated by the intergranular pores, with an average porosity of 10.29% and an average permeability of 34.12×10-3 μm2. In general, it belongs to the category of low porosity and low permeability reservoirs with limited development of some medium-high porosity and permeability reservoirs. The diagenesis of the reservoir mainly includes compaction, cementation, and dissolution, and the diagenesis intensity is relatively weak. The main body is at the early diagenesis (stage B) to middle diagenesis (stage A), and it is characterized by medium compaction intensity, low cement content, and acid dissolution at the late stage. In particular, the characteristics of enriched quartz and feldspar, poor cuttings, and good sorting are conducive to the preservation of reservoir physical properties.

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    REE Geochemistry and Its Environmental Significance of Subsurface Black Soil from Northwestern Arongqi, Songnen Plain Black Soil District
    DU Guanxin, YAN Baiquan, SUN Yu, QIAN Cheng, QIN Tao, ZANG Yanqing
    Geoscience    2023, 37 (03): 813-820.   DOI: 10.19657/j.geoscience.1000-8527.2022.098
    Abstract170)   HTML3)    PDF(pc) (1659KB)(93)       Save

    Formation of black soil in Northeast China has long been a research focus in the academia, but anthropological activities have influenced the study of surficial black soil to varying degrees. At present, there is a paucity of research on the underground black soil. In this study, the black soil from drill-cores at Arongqi of the Songnen Plain was sampled for REE geochemical analysis. Distributions of ΣREE, HREE and LREE elements of the deep black soil layer were analyzed by geostatistics. Combined with the Ce anomaly, Eu anomaly, (La/Yb)N, (La/Sm)N, (Gd/Yb)N, Al2O3 vs. TiO2 diagram and Ceanom, the provenance and formation environment of the black soil are discussed. The results show that the subsurface black soil at Arongqi have high ΣREE content (avg. 141.45 mg·kg-1). The right-inclining chondrite-normalized patterns show LREE enrichments, with weak negative Eu and strong negative Ce anomalies. The average (La/Yb)N =7.58, (La/Sm)N=1.14, and (Gd/Yb)N=3.54, indicating that the HREEs and LREEs are highly fractionated, and the LREE fractionation is stronger than that of HREE. The δEu and Al2O3/TiO2 diagram indicate that the subsurface black soil was sourced from the nearby Cretaceous felsic-intermediate magmatic rocks. The Ceanom >-0.1 (mean 3.9)suggests an anoxic environment.

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    Topography and Fractal Characteristics and Their Genesis of the Wudalianchi Volcanic Group in Heilongjiang
    WANG Jinyu, LIU Yongshun, PAN Meihui, NIE Baofeng, ZOU Wang, LU Zhi, ZHANG Xinyi
    Geoscience    2024, 38 (03): 793-806.   DOI: 10.19657/j.geoscience.1000-8527.2024.001
    Abstract165)   HTML15)    PDF(pc) (18437KB)(231)       Save

    Volcanic topography is essential to study the formation of volcanoes and evolution of planetary morphology.Based on the remote sensing images and DEM data of the Wudalianchi volcanic area, we analyzed fractal characteristics and performed the comprehensive interpretation in its formation, and discussed the complex genetic mechanisms of the geomorphic system in this volcanic area.The results show that (1) volcanic cones and lava topography constitute the surface morphology with low undulation frequency in the area, and the number of composite volcanic cones distributed along the fractures affects the topographic complexity in this direction.(2) The topography of this area shows a fractal structure of multiscale domains and a small fractal dimension (D≈2), which was presumably influenced by the extensive lava topography and low volcanic cones.The fractal dimensions of the topographic profiles in the directions of fractures show that the geomorphic anisotropy of the three fracture directions in the Wudalianchi volcanic area is relatively small (D=1.142-1.275), and the difference between Dmax and Dmin is only 0.133.However, the fractal dimensions in the NE direction are large (DNE=1.223-1.275), which is the principal fracture direction affecting the volcanic topography.(3) The topographic characteristics of the volcanic group are determined by internal and external agents, and two sets of fractural structures (deep and shallow fractures) and magmatic systems are the main factors affecting its topographic features at the present stage.The role of external agent in stochastic coarsening at the meso-to-micro scale is intensifying, but synergistic antagonism has not yet prevailed at the macro scale, and the complex regional topography of the volcanic group has not yet changed.Remote sensing spectral features and topographic analyses are effective to investigate the volcanic topography, and the quantitative fractal characteristics can interpret the topographic characteristics at different scales and becoming a novel approach to study volcanic topography and their genesis.

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    Spatiotemporal Evolution and Assessment of Ecological and Geological Environment Safety in the Upper Reaches of the Minjiang River from 1995 to 2020
    JI Yang, BA Renji, XIAO Chengzhi, LIU Lei, ZHOU Xueni, CAO Yating
    Geoscience    2024, 38 (03): 648-659.   DOI: 10.19657/j.geoscience.1000-8527.2024.037
    Abstract160)   HTML18)    PDF(pc) (12852KB)(198)       Save

    The upper reaches of the Minjiang river are key barriers of ecological safety in the upper reaches of the Yangtze river. Since the Wenchuan earthquake in 2008, the underground rock masses, surface matrix, and aboveground ecology were severely damaged. To investigate the status of ecological and geological safety in the upper reaches of the Minjiang river before and after the earthquake, we selected 16 evaluation indicators from the two dimensions of “geological environment-ecological environment”. We also evaluated the ecological and geological environment safety of the upper reaches of the Minjiang river basin in 1995, 2001, 2009, and 2020 based on the AHP-PCA entropy-combination weight method, and furthermore analyzed its evolution trend. The results indicate that the overall ecological and geological environments in the upper reaches of the Minjiang river basin are generally safe. Specifically, the ecological and geological environments are relatively safer in the central and eastern regions of the basin, while the relatively less safe or unsafe regions are mainly distributed in the western and northern high mountain areas and deep valley areas. This presents a general pattern of high safety in the central and eastern regions and low safety in the western and northern regions. From 1995 to 2020, the overall ecological and geological environment safety in the upper reaches of the Minjiang river showed a trend of decreasing at the beginning and then gradually increasing. The ecological and geological environment safety in the northern and deep valley areas of the watershed fluctuates greatly, showing an increasing-decreasing-increasing trend and unstable ecological and geological environments. The overall safety of the ecological and geological environments in the southwest is reduced after the earthquake. Although the reduced area gradually decreases, the overall ecological and geological environments continue deteriorating. The overall safety of the ecological and geological environments in the central part of the basin is generally increasing and the area is gradually increa-sing. The results of this study provide theoretical basis for the ecological protection and restoration in the upper reaches of the Minjiang river.

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    Identification and Significance of Early Cretaceous Highly Fractionated Alihe Granites, Northern Great Xing’an Range
    XU Liming, LIU Tao, ZHENG Jilin
    Geoscience    2023, 37 (03): 613-626.   DOI: 10.19657/j.geoscience.1000-8527.2021.053
    Abstract154)   HTML15)    PDF(pc) (7461KB)(114)       Save

    There are voluminous Mesozoic granitic rocks in the Great Xing’an Range. In this study, zircon U-Pb geochronology and geochemistry of the Alihe granites in the northern Great Xing’an Range were analyzed, and were compared with the Mesozoic granites in the northern, middle and southern Great Xing’an Range and South China. The petrogenesis and tectonic setting of the Alihe granites were then discussed. Zircon U-Pb dating on two granite samples yielded Early Cretaceous ages (134.6±1.5 Ma and 134.4±1.0 Ma). The Alihe granites are mainly composed of monzogranite, syenogranite, and alkali-feldspar granites, which contain few mafic mi-nerals and miarolitic cavities. Alaskite and aplite were found in the field investigation route and pegmatite veins were found on the granitic pluton margin. Chemically, these plutons are peraluminous (A/CNK=1.01-1.11) and show high contents of SiO2 (73.63%-77.81%), alkalis (Na2O+K2O=7.78%-8.97%), and DI (91.71-96.80), and low Ca and Mg contents. They are also enriched in Rb, Th, U, K, but depleted in Nb, Ta, P, Ti. The varying Zr/Hf and Nb/Ta ratios resemble highly-fractionated granites in South China. Integrating geological and geochemical data, we suggested that the Alihe plutons are highly fractionated I-type granites, which were formed in a post-orogenic extension setting after the Mongolia-Okhotsk Ocean closure.

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    Geochronology, Geochemistry and Geological Significance of Tuanbaoshan Metamorphic Rocks in Haiyan, Qinghai Province
    WANG Xiangwei, ZHANG Baotao, YANG Haoqiang, HAN Jinguo
    Geoscience    2023, 37 (03): 586-598.   DOI: 10.19657/j.geoscience.1000-8527.2021.149
    Abstract153)   HTML9)    PDF(pc) (7076KB)(130)       Save

    The Tuanbaoshan metamorphic rocks (Hualong Group) are widely distributed in eastern South Qilian (Haiyan County, Qinghai Province). To deepen our understanding on the local metamorphic rocks and their geological significance, analyses of petrography, geochronology and geochemistry were conducted on the least-altered samples. The obtained weighted average ages ((2,047±30) Ma and (755±13) Ma) indicate that the formation age is Late Proterozoic. The average chemical content of the rock: SiO2 accounts for 62%, FeO accounts for 4.79%, Fe2O3 accounts for 6.44%, MgO accounts for 3.46%, and the average total amount of rare earth elements is 476×10-6. The rocks right-inclining chondrite-normalized REE and flat HREE patterns, weak Eu anomalies and LREE enrichment. The metamorphic rocks are rich in high field strength elements (HFSEs, e.g., Th, U, Ce, Zr, and Hf), but depleted in lithophile elements (e.g., Ba, P, and Ti). Comprehensive geochronological and geochemical characteristics suggest that protoliths of the local metamorphic rocks are mainly felsic sandy mudstone, and the protolithic formation environment may have been continental arc associated with the Rodina supercontinent breakup.

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    Sedimentary Environment of the Phosphorus-bearing Layers and Its Phosphate Enrichment Mechanism of the Cambrian Xinji Formation, Western Henan
    JIA Bingling, ZHANG Biyun, TANG Bin, ZHENG Deshun
    Geoscience    2023, 37 (04): 858-869.   DOI: 10.19657/j.geoscience.1000-8527.2022.094
    Abstract153)   HTML19)    PDF(pc) (10935KB)(489)       Save

    The Cambrian is an important period for global phosphate deposition, and the Cambrian Xinji Formation is an important phosphorus-bearing sequence on the southern margin of North China Craton. However, the relationship between the phosphorus-bearing stratigraphy and the sedimentary environment is poorly understood, and the phosphate enrichment mechanism needs to be further studied. Here, we studied the middle Xinji Formation at Baofeng, which contains a typical phosphorus-bearing layer. Field observations and laboratory analyses were conducted to reveal its depositional environment and explore its phosphorus source and enrichment mechanism. The results show that phosphorus nodules from the Xinji Formation are black, irregular flat disk-shaped, with size of 2 to 20 mm, and are distributed in the fine sandstone beds. Collophanite is the main mineral in the nodules. There are two forms: (1) cryptocrystalline rounded colloidal phosphorite with no internal structure and locally cracked; (2) microcrystalline oolitic colloidal phosphorite with fine veins. The depositional environment of the Xinji Formation was likely littoral-shallow marine transition. Phosphorus was likely derived from deep oceanic phosphorus-rich water and small shell biological activities. Formation of the phosphorus nodules was likely dominated by chemical deposition with indirect biological involvement. It has undergone syn-deposition and early diagenesis stages, and large amounts of phosphorus nodules were deposited in turbulent shallow water. Compared with the Cambrian phosphorus-bearing facies in the Yangtze Craton, the phosphate-bearing stratigraphy is clearly diachronic, and phosphate deposition occurred after the sedimentary hiatus. Initial deposition of the Cambrian phosphate was dominated by biological and chemical processes, and then the depositional environment and paleotectonics controlled the phosphorus-bearing stratigraphy and promoted the re-enrichment. We point out the relationship between phosphorus enrichment and the Early Cambrian sedimentary environment in the southern North China Craton, and provide abundant data for studying large-scale phosphate deposition.

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    Development and Evolution Characteristics of Strike-slip Faults in Tarim Basin and Its Geological Significance: A Case Study of F17 Fault in Fuman Oilfield
    LIU Qiang, ZHANG Yintao, CHEN Shi, SONG Xingguo, Li Ting, KANG Pengfei, MA Xiaoping
    Geoscience    2023, 37 (05): 1123-1135.   DOI: 10.19657/j.geoscience.1000-8527.2023.058
    Abstract150)   HTML22)    PDF(pc) (16110KB)(256)       Save

    The strike-slip fault in the platform Tarim basin has the characteristics of “controlling reservoir, controlling reservoir and controlling wealth”, but because it is developed in ultra-deep layer and its activity intensity is low, the fine analysis and evolution characteristic analysis of the fault is the focus and challenge of the current research.To deepen the fine analysis process of strike-slip fault structure and explore the geological significance of fault activity, we took F17 fault as a case study.Based on the new high-precision 3D seismic data in the Fuman oilfield, combined with a variety of seismic attributes such as coherence, maximum likelihood and reservoir amplitude change rate, we analyzed the spatial distribution regularity, activity characteristics and evolution process of faults, and the characteristics of fault control and storage in combination with the reservoir development characteristics.Based on the reconstruction of the local structural characteristics of the Precambrian basement, the development mechanism of fault plane strike migration is preliminarily analyzed.The results show that the local F17 fault plane has changed many times and its strike shifted counterclockwise from south to north.Based on the changing characteristics of the fault strike, the fault can be divided into three segments: North (NE8°), middle (NE33°) and south (NE50°).The fault has the characteristics of vertical delamination defor-mation.According to the fault deformation characteristics, it can be divided into the deep structural deformation layer characterized by vertical strike-slip (below TO3t), and the shallow structural deformation layer with echelon normal fault (above TO3t).The fault has the characteristic of “stratified flowering” in the deep structural deformation layer, and several flower-like structures are developed vertically, which are mainly distributed near the bottom of the Upper Cambrian (T∈3) and the top of the Yijianfang Formation (TO3t).Three groups of echelon normal faults are developed vertically in the shallow structural layer, which are distributed in TO3t-TS, TS-TC and TC-TT from bottom to top.The fault evolution is likely multi-stage, and the evolution can be divided into five stages: early Caledonian, middle Caledonian Ⅰ, middle Caledonian Ⅲ, late Caledonian-early Hercynian, and middle-late Hercynian.The Precambrian basement rift structure likely affected the development and connection of the overlying strike-slip faults, resulting in the fault plane offset.

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    Lajia Ruins in Qinghai Province Might Be Caused by Seismic-induced Liquefaction Mudflows of Sands and Soils: Implication from the Jishishan Earthquake in Gansu Province on December 18, 2023
    LI Junlei, ZHANG Xujiao, YU Hailin, WANG Yifan, ZHANG Xiangge, LI Qiurong, LI Caihong, ZHANG Lilei
    Geoscience    2024, 38 (01): 248-259.   DOI: 10.19657/j.geoscience.1000-8527.2024.012
    Abstract149)   HTML15)    PDF(pc) (17149KB)(125)       Save

    The Lajia Ruins, often called the “Pompeii in the East”,situated in Minhe County, Qinghai Province, is well known as an archaeological site documenting a catastrophic event approximately 3,900 years ago. The causation of the disasters responsible for the destruction of the Lajia settlement has been in hot debate for an extended period. Various points of view regarding “flooding causes” has been gained acceptance within the general public. However, is the catastrophic event indeed linked to flooding? The 6.2-magnitude earthquake struck in Jishishan County, Gansu Province on December 18, 2023, with its epicenter located a mere 16 kilometers from the Lajia Ruins. This seismic event not only substantially damaged the Lajia Ruins Museum but also triggered mudflows in Jintian Village and Caotan Village, Zhongchuan Town, Minhe County, just 5 kilometers away from the Lajia Ruins. This catastrophic event led to the direct burial of residential structures and villagers, potentially representing a replication of the formative processes that gave rise to the Lajia Ruins. Consequently, it emerges as a pivotal empirical material for comparative studies investigating the causative factors underlying the genesis of the Lajia Ruins. Through conducting field investigations and comprehensive studies of the seismic disaster, it is conceivable that contemporary insights may shed light on the longstanding enigma surrounding the genesis of the Lajia Ruins. The earthquake has induced an upward surge of groundwater from the ancient riverbed gravel layers beneath the loess, causing the liquefaction of the loess and the rapid downstream flow of mud through gullies. As the mudflow encountered obstacles when passing through Caotan Village and Jintian Village, it overflowed the gullies, destroying some houses and even burying villagers. The distinctive geological stratigraphy and the abundance of groundwater, triggered by seismic activities, resulted in soil’s liquefaction and mudflows’ formation, constituting crucial factors in the genesis of seismic disasters in Zhongchuan Town. Field investigations indicated the tragic burial of a family of five in Caotan Village was not the result of a typical “sand surge”, nor does it exhibit traces of “flooding”. Instead, it is attributed to secondary seismic hazards, specifically mudflows induced by the earthquake. Combined with the preservation status of cultural remains and sedimentary characteristics at the Lajia Ruins, inference suggests that the ancient earthquake 3,900 years ago, along with the resultant liquefaction of soil and the rapid flow of mud, provides a plausible explanation and reconstruction for the instantaneous catastrophe at the Lajia Ruins. The formation of the Lajia Ruins is likely unrelated to the mountainous flash floods induced by heavy rainfall and certainly not caused by the purported megaflood.

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    Spatial and Temporal Variability of Carbon Stocks in Different Land-use Types in the Yiluo River Basin in the Middle Section of the Yellow River from 1990 to 2050
    YUAN Jianglong, LIU Xiaohuang, LI Hongyu, XING Liyuan, LUO Xinping, WANG Ran, WANG Chao, ZHAO Honghui
    Geoscience    2024, 38 (03): 559-573.   DOI: 10.19657/j.geoscience.1000-8527.2024.035
    Abstract148)   HTML22)    PDF(pc) (11841KB)(229)       Save

    The change of land-use type is the key influence factor of regional carbon stocks, which significantly affects the whole terrestrial ecosystem. Taking the Yiluo River Basin in the middle section of the Yellow River as an study case, we assessed the spatial and temporal variations and influence factors of carbon stocks based on the Integrated Valuation of Ecosystem Services and Trade-offs (InVEST) model during 1990—2020. We predicted the land-use types and carbon stock using the coupled PLUS model for the period of 2025-2050. A geoprobe was used to explore the regional carbon stock driving factor. The results show that (1) the land-use types in the Yiluo River Basin shifted to transferring-out with cropland and grassland, and transferring-in with forest land, water-body, and construction land. The regional carbon stock increased by 1.0×107 t from 1990 to 2020, with a continuous drop of carbon stock in the east and a continuous increase in the central and western areas. (2) The predicted overall regional carbon sequestration capacity decreases from 2025 to 2050. Comparing with the historical period, the carbon sequestration capacity in the east continues to decline and the carbon sequestration capacity in the central and western areas changes from a continuous increasing to a trend of overall increasing. the environmental restoration scenario is the most favorable to regional carbon sequestration, while the cultivated land protection scenario is the most unfavorable. (3) The geoprobe results indicate that the q-value (explanatory power) of Normalized Vegetation Index (NDVI) in the one-way analysis is 0.561, which has the strongest explanatory power. The q-value of Digital Elevation Model interacting with NDVI in the analysis is 0.592, showing a stronger explanatory power. It is recommended that the economic and agricultural development in the regions with a better economy and flat region (IV12-1) should emphasize the protection of nature. The regions with a better ecology and high altitude (VI22-1 and VI22-3) is recommended to mainly implement the ecological restoration strategy.

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    Progress on Metallogenic Research of Granite-related Uranium Deposits from Luzong Ore District in the Middle and Lower Reaches of Yangtze River Metallogenic Belt
    ZHANG Shu, ZHANG Zanzan, HU Zhaoqi, SHI Lisheng, ZHOU Taofa, WU Ming'an, DU Jianguo
    Geoscience    2023, 37 (06): 1435-1448.   DOI: 10.19657/j.geoscience.1000-8527.2023.083
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    The Lujiang-Zongyang ore district is one of the most important ore cluster regiones in the Middle and Lower Reaches of the Yangtze River Metallogenic Belt, and is also an important uranium prospecting area in the South China Uranium Province.Systematic uranium metallogenic study would benefit the understanding of the regional metallogenic theory and uranium prospecting.In this paper, we provide a review of the geological features, uranium-bearing intrusions, magmatic and metallogenic ages, ore-forming fluids, and uranium sources of the typical uranium deposits in the Lujiang-Zongyang ore district.The uranium deposits along the NE-trending A-type granite belt are controlled by intrusive contact, faults, and interlayer structures.The uranium deposits were formed at 114-108 Ma, whereas the ore-bearing granites are A1-type and were formed at 127-123 Ma with 115-110 Ma alkali feldspar granitic stocks.The ore-forming materials were derived from the ore-bearing intrusions and wall-rocks.The ore-forming fluids were the mixture of magmatic water and meteoric water.The uranium was likely originated from the leaching of the ore-bearing intrusions during the fluid circulation, and deposited by changes in the physicochemical condition.The uranium mineralization in the Luzong basin was controlled by concealed syenite and was formed at 131-129 Ma.The ore-bearing intrusions, which provide the ore-material sources, are of shoshonitic and were formed at 131 Ma.The ore-forming fluids were mainly of magmatic water.The uranium was probably fractionated from the F-B-rich melt into the magmatic fluids, and uraniferous veins were formed as the pressure and/or temperature dropped.We suggest that the granite uranium fertility indicator, high-precision dating of uranium deposits, and the genetic link between mantle-derived material and uranium mineralization are important research topics in future.

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    Characteristics and Geological Significance of Geoheritage in the Arxan Global Geopark, Inner Mongolia
    WANG Lulin, ZHU Qingfeng
    Geoscience    2023, 37 (04): 1075-1088.   DOI: 10.19657/j.geoscience.1000-8527.2023.086
    Abstract146)   HTML8)    PDF(pc) (7279KB)(594)       Save

    The scientific classification and characterization of geoheritage is the premise and foundation of rational utilization and protection of geoheritage. The Arxan Global Geopark has distinctive and extremely rich geoheritage, which has high touristic value and geological research significance. In this paper, based on geolo-gical survey and evaluation of the geoheritage, we divided the geoheritage resource into two categories,i.e. geomorphological landscape and water landscape,and six landform/landscape types,i.e. volcanic, rock, fluvial, structural, and spring water,and 9 subcategories,i.e. volcanic formation, volcanic lava landform, volcanic lake, granite landform, fluvial erosion landform, fluvial accumulation landform, structural landform, hot spring, and scenic river sections, with 47 geosites in total. Among them, volcanic landforms and hot spring landscapes are of great significance in the comparative analysis of global geoheritage. Additionally, the authors analyzed the characteristics of various geoheritage and discussed the important geotouristic significance of the geoheritage in the Arxan Geo-park. Studies have shown that the geoheritage of Arxan Geopark have important scientific value in the fields of geomorphology, hydrogeology and geotourism. This provides a scientific basis for the protection of geoheritage and tourism route planning, and promotes the sustainable development of geoscience research, science popularization and geoscience tourism in the Arxan Geopark.

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    Detrital Zircon U-Pb Age and Hf Isotopes and Their Geological Significance of the Nenjiang River Floodplain Sediments
    LIANG Qiankun, CHEN Yuelong, WANG Shanhui, YU Yang, YANG Fan
    Geoscience    2023, 37 (03): 529-546.   DOI: 10.19657/j.geoscience.1000-8527.2022.036
    Abstract145)   HTML19)    PDF(pc) (6291KB)(127)       Save

    In this study, we conducted LA-(MC)-ICP-MS U-Pb dating and Hf isotope analysis on detrital zircons from the Nenjiang River floodplain sediments. The results show that the U-Pb ages of 293 detrital zircons can be divided into four major groups, i.e., 2,300-1,746 Ma, 363-331 Ma, 316-260 Ma, and 252-86 Ma. Mesozoic detrital zircons account for 80.9% of the total amount, indicating strong magmatism in the source region during this period. The relative outcrop size of strata (of different ages) is different in the basin: Jurassic-Cretaceous (~72%), Carboniferous-Permian (~13%), Triassic (~8%), Precambrian (~5%), and Cambrian-Silurian (~1%). The Hf isotope composition may reflect the formation and evolution of continental crust in the Nenjiang River catchment. Continental crust in the Nenjiang River basin is mainly produced by juvenile crust formation. The ca. 1,200-400 Ma period likely represents a major continental growth event in NE China, which formed 98.8% crustal components of the present crust, which may be related to the Paleo-Asian Ocean development and subduction. During ca. 400-100 Ma, the Nenjiang Basin may have experienced intense intra-continental crustal recycling. Furthermore, using the formula of recycling ratio, the remelting vs. juvenile crust ratios have been calculated. The Mesozoic zircon have a low remelting ratio and contain about 70% juvenile crust. This phenomenon is related to the partial melting of mantle material caused by subduction of the Mongol-Okhotsk Ocean and Paleo-Pacific Ocean.

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    Arsenic-Uranium Distribution Characteristics and Risk Assessment in the Aquatic Environment of Hailar Basin
    LIU Shengfeng, GAO Bai, YI Ling, FANG Zheng, SHI Tiancheng, DING Yan
    Geoscience    2023, 37 (04): 933-942.   DOI: 10.19657/j.geoscience.1000-8527.2022.020
    Abstract143)   HTML3)    PDF(pc) (7500KB)(86)       Save

    The Hailar Basin is located in an arid to semi-arid region, and its water resource has received widespread attention. Studying the hydrogeochemical characteristics of the local water environment and health risk assessment is conducive to better protection and utilization of water resource. Based on field sampling data, we analyzed its hydrochemical characteristics and influence factors, used the PHREEQC software to simulate the As-U occurrence, and conducted characteristic analysis and risk assessment of As-U co-pollution phenomena. The results show that the As-U concentrations in the local water environment mostly exceed the World Health Organization (WHO) standard limits. The As concentration in the water environment in the Beier Lake Depression-Cuogang Uplift is higher, and the U concentration in the Cuogang Uplift near Hulun Lake is higher. Calculated by the US EPA health risk assessment model, the average non-carcinogenic total risk HItotal of different populations all exceed the acceptable level (HItotal <1), and the average carcinogenic risk of As also exceeds the acceptable level (1×10-6). The total non-carcinogenic risk and carcinogenic risk: children>female adult>male adult. The PHREEQC simulation results show that As in the water environment mainly exists in the form of As(V), and most of the sampling spots are dominated by HAsO 4 2 - and H2 AsO 4 -. Uranium occurs mainly in the form of U(VI): UO2(CO3) 3 4 - and UO2(CO3) 2 2 -. The chemical valence of As is readily affec-ted by the pH and Eh values. The pH decrease and the more toxic As(III) are likely formed under relatively reducing conditions. The chemical valence of U is not strongly affected by the pH and Eh values, but changing which would also form solid deposits such as bituminous uranium ore, which may cause stones and other related diseases.

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    Key Issues and Reflections on the Systematic Observations and Research System for Natural Resources
    LIU Xiaohuang, XIONG Maoqiu, MIN Jie, YUAN Jianglong, CHEN Wudi, YAN Yuxiang, LI Zhiheng
    Geoscience    2024, 38 (03): 549-558.   DOI: 10.19657/j.geoscience.1000-8527.2024.020
    Abstract143)   HTML33)    PDF(pc) (13657KB)(414)       Save

    Natural resources are the material basis of industrial production and citizen living, hence appropriate exploitation and protection of natural resources have been a long-standing task. Inappropriate exploitation and utilization of natural resources will lead to deterioration of the ecological environment and will affect the econo-mic development. To construct a systematic observations and studies towards an unified management of natural resources, we investigated the relationship between observations and studies of the natural resources and ecosystems, and the relationship between investigation and monitoring. We also selected some sites for systematic field observation and determined the operation mechanism and the issues of concerns to the industries. We also summarized a framework of constructing an observation system and received the results of the pilot observations and investigations. Consequently, we put forward the opinions and suggestions on solving the issues of the construction of the proposed system. The study results provide inspirations and recommendations on constructing an integrated observation and research system for natural resources.

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    Variation Regularity of Groundwater Level in the Yongding River Basin Under Ecological Replenishment
    HU Xinyu, SHEN Yuanyuan, CHU Tingwen, HE Wei, WEI Wei, SHEN Xiaopeng
    Geoscience    2023, 37 (04): 986-993.   DOI: 10.19657/j.geoscience.1000-8527.2021.155
    Abstract141)   HTML10)    PDF(pc) (9825KB)(132)       Save

    In the spring of 2020, the ecological water replenishment in Yongding River Basin (Beijing section) was officially started on the 20th of April. To understand the variation regularity of groundwater level in the Beijing section of the Yongding River basin and the surrounding areas under the influence of ecological water replenishment, based on the observation data of groundwater level within six months after the spring water reple-nishment in 2020, the data were classified by clustering method. Subsequently, each type of variation regularity was analyzed separately. The results show that the dynamic change types of groundwater level in Yongding River Basin under the ecological water replenishment influence can be divided into (1) continuous decline type, (2) decline type and then increase, and (3) continuous constant type, among which the groundwater level in the Beijing section, Tianjin section, and part of Hebei section shows type 2, and there is an obvious lag. However, the other parts of the Hebei section and Shanxi section show type 3, and only a few sites show type 1. These regularities can provide a technical reference for making scientific ecological water replenishment scheme.

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    Zircon U-Pb Isotopic Geochronology,Bulk Geochemistry and Their Geological Significance of the Quartz Monzodiorite from the Taibaihe Region in the South Qinling Orogen
    WANG Ruiting, LI Qingfeng, QIN Xishe, ZHANG Bin, WANG Bowen, JI Yuefei
    Geoscience    2023, 37 (03): 562-572.   DOI: 10.19657/j.geoscience.1000-8527.2023.013
    Abstract139)   HTML19)    PDF(pc) (7090KB)(337)       Save

    In order to ascertain the formation time, petrogenesis, magma source and tectonic setting of the intermediate rocks in Taibaihe area of South Qinling, zircon U-Pb geochronology and geochemistry of the quartz monzodiorite have been studied in the thesis. The results of LA-ICP-MS zircon U-Pb gechronology show that the 206Pb/238U weighted mean age of quartz monzodioirte is (216.8±2.2) Ma (MSWD=1.15,n=20), indicating that it was formed in the Late Triassic. According to the lithogeochemistry studies, the quartz monzodioirte belongs to the aluminum unsaturate and high potassium calc-alkaline series. This suite of rocks are rich in LILE (such as K, Rb) and HFSE (such as Zr, Hf), and relatively depleted in Nb, Ta, P, and Ti. The quartz monzodiorite is rich in LREE and poor in HREE, with slightly negative Eu anomalies. The magma source has the characteristics of crust-mantle mixed molten. Based on the tectonic evolution of the South Qinling Orogen, we consider that the Taibaihe quartz monzodioirte may be formed in the syn-collisional to post-collisional stage of the orogeny, belonging to the product of same homologous magmatism activity as Xiba granites. According to the previous studies of regional magmatism, tectonic activity and mineralization, and the new work of magmatic-metallogenic ages modification in our study, it is considered that the metallogenic age of Fengtai ore cluster region is Late Triassic.

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    Geochemical Characteristics of Heavy Metals in Soils and Soil Quality Evaluation of Green Food Production in the Yongqing County of Beijing-Tianjin-Hebei Region
    HU Qinghai, WANG Xueqiu, HAN Zhixuan, CHENG Xiaomeng, WU Hui, TIAN Mi, LIU Futian, SUN Binbin, CHEN Weiming, DU Xuemiao, LIU Bin, CUI Xingtao
    Geoscience    2023, 37 (03): 778-789.   DOI: 10.19657/j.geoscience.1000-8527.2023.015
    Abstract138)   HTML5)    PDF(pc) (6586KB)(219)       Save

    To ensure food safety in the Beijing-Tianjin-Hebei region, the Yongqing County (Langfang City, Hebei Province) was selected as the research area. A total of 412 surface and 410 deep soil samples were collected to determine the concentration of eight heavy metals, i.e., As, Cd, Cr, Cu, Hg, Ni, Pb and Zn. Meanwhile, the enrichment factor and potential ecological risk were used to evaluate the degree of heavy metal pollution and ecological risk. The results showed that the average concentrations of eight heavy metals in surface (deep) soil in Yongqing region are As 9.44 mg/kg (8.93 mg/kg), Cd 0.16 mg/kg (0.10 mg/kg), Cr 64.4 mg/kg (62.3 mg/kg), Cu 24.6 mg/kg (20.7 mg/kg), Hg 0.41 mg/kg (0.20 mg/kg), Ni 27.7 mg/kg (27.7 mg/kg), Pb 20.7 mg/kg (18.2 mg/kg) and Zn 72.8 mg/kg (57.5 mg/kg), respectively. The spatial distribution of heavy metal concentration shows a pattern of high in the southwest and low in the northeast. Based on the enrichment factor (EF), the eight heavy metals could be divided into three categories: (1) Hg (2.18) is strongly influenced by human activities; (2) Pb (1.14), Cu (1.22), Zn (1.29) and Cd (1.63) are controlled by natural geological background and human activities; (3) Ni (1.01), Cr (1.05) and As (1.09) are mainly controlled by natural geological background. Results of the environmental quality assessment showed that the local soil is largely safe to use, and the risk area is only 1.1 km2, accounting for 0.14% of the total area. The area that meets the evaluation standards for green food production is about 756.62 km2, accounting for 99.43% of the total area. Among them, the area of irrigated land, dry land, orchards in accordance with the standard accounted for 98.94%, 99.29% and 99.59% of the total area of their respective land categories. In terms of ecological risk, the soil comprehensive ecological risk index of the local dryland, irrigated land and orchard agricultural land is largely low, accounting for 95.63%, 77.37% and 98.35%, respectively. Only dry land (0.13 km2) and irrigated land (0.03 km2) have a few higher ecological risk areas, which deserve further ecological evaluation. In conclusion, although heavy metal contents in some areas at Yongqing are affected by human activities, most areas have low ecological risk. In this study, the area that meets the evaluation standards for green food production and low comprehensive potential ecological risk is determined as the most suitable for large-scale green food production. This area is 669.12 km2, accounting for 87.93% of the total area. Our results provide a scientific basis for local production, planting and planning management of green agricultural products.

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    Identification of Strike-Slip Faults and Exploration Breakthroughs in the Fuman Area, Tarim Basin
    ZHANG Yintao, YU Yixin, XIE Zhou, SUN Chong, WANG Xiaopeng, SHEN Biao, DU Qirui
    Geoscience    2024, 38 (06): 1417-1430.   DOI: 10.19657/j.geoscience.1000-8527.2024.065
    Abstract135)   HTML17)    PDF(pc) (15210KB)(205)       Save

    Strike-slip fault zones well-developed in the Fuman area within the Aman transition zone of the Tarim Basin. These faults significantly impact the reservoir characteristics and hydrocarbon accumulation in the Ordovician carbonate rocks. However, identifying strike-slip faults in the Fuman area remains challenging. Using new 3D seismic data from the Fuman area, this study has identified and characterized primary and secondary strike-slip faults through multiple filtering, coherence analysis, and signal decomposition techniques. Additionally, a quantitative standard for classifying strike-slip faults has been established. Furthermore, the exploration potential of the strike-slip faults has been evaluated using the “three determination” approach. The results show that 70 large-scale strike-slip faults are developed within the Tabei Uplift and Central Uplift belts. Based on their development lengths, activity periods, and intensity, the primary strike-slip faults are classified into Class I (25 faults) and Class II (45 faults). In the Fuman area, 34 major strike-slip faults have been identified. Based on fault characterization and drilling data, the “three determination” method, encompassing the determination of faults system, fracture-cavity boundaries, and reservoir units, is proposed for evaluating resources in the Ordovician carbonate reservoirs. The resources associated with the 70 strike-slip faults include 20×108 t of oil and 1×1012 m3 of gas, with 11×108 t of oil located specifically in the Fuman area. Based on detailed characterization of the strike-slip faults, three new structural belts with abundant oil and gas resources have been identified and confirmed by wells. The study indicates that strike-slip faults of various scales in the Fuman area hold significant potential for increasing reserves and production. This study not only advances research on strike-slip faults and the exploration of fault-controlled fractured-vuggy carbonate reservoirs in the Tarim Basin platform area but also provide valuable guidance for studying strike-slip faults in other cratons.

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    Geochronology, Geochemistry and Geological Significance of the Huatugou Intermediate-acid Intrusions at Qimantag, Xinjiang
    MA Decheng, XI Zhen, GAO Guangming, LI Huan
    Geoscience    2023, 37 (03): 599-612.   DOI: 10.19657/j.geoscience.1000-8527.2022.041
    Abstract134)   HTML8)    PDF(pc) (7241KB)(237)       Save

    The Qimantag in East Kunlun orogen has strong magmatic activity from the Silurian to Devonian, and its formation is related to oceanic lithosphere subduction orogeny and collision-post-collision orogeny. In this paper, zircon U-Pb chronology and whole-rock major and trace element geochemistry are carried out on the Hua-tugou granodiorite in Qimantag, and the petrogenesis and tectonic background are discussed. LA-ICP-MS zircon U-Pb dating of the granodiorite is (396.5±4.6) Ma, which is the product of Early-Middle Devonian magmatic activity. The whole-rock SiO2 content is 63.01%-74.70%, showing characteristics of high K2O (1.53%-4.01%), Na2O (2.16%-3.80%) and Al2O3 (12.95%-14.48%), Mg# is 17.01-61.23, belonging to calc-alkaline and high-K calc-alkaline series. The chondrite-normalized REE patterns are moderately right-dipping and smooth, with negative Eu anomaly (δEu=0.48-0.72). Trace element spider diagram shows that the rocks are enriched in large ion lithophile elements (LILEs), such as Rb, Th, La, Ce and light rare earth elements (LREEs), and is depleted in Nb and Ta, Ba and other high field strength elements (HFSEs), belonging to I-type granite. Combined with the magmatic age, geochemical characteristics and regional tectonic evolution, we considered that the granodiorite is the partial melting product of orogenic crustal materials (especially accretionary crustal materials), mixing with some mantle-derived material, and experienced fractionation of feldspar and other minerals during the magma evolution. The tectonic regime may have been a compression-extension transition from syn-collisional to post-collisional setting.

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