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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
    Abstract515)   HTML8)    PDF(pc) (12188KB)(217)       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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    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
    Abstract264)   HTML7)    PDF(pc) (6485KB)(67)       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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    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
    Abstract222)   HTML4)    PDF(pc) (4917KB)(123)       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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    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
    Abstract222)   HTML5)    PDF(pc) (2408KB)(55)       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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    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
    Abstract213)   HTML16)    PDF(pc) (12425KB)(161)       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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    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
    Abstract190)   HTML4)    PDF(pc) (6091KB)(87)       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
    Abstract187)   HTML7)    PDF(pc) (8511KB)(114)       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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    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
    Abstract178)   HTML2)    PDF(pc) (7945KB)(79)       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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    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
    Abstract157)   HTML3)    PDF(pc) (1659KB)(39)       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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    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
    Abstract152)   HTML27)    PDF(pc) (12773KB)(281)       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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    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
    Abstract140)   HTML5)    PDF(pc) (10155KB)(70)       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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    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
    Abstract139)   HTML8)    PDF(pc) (7461KB)(48)       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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    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
    Abstract137)   HTML18)    PDF(pc) (4559KB)(257)       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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    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
    Abstract129)   HTML5)    PDF(pc) (7076KB)(58)       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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    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
    Abstract123)   HTML5)    PDF(pc) (6586KB)(103)       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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    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
    Abstract122)   HTML19)    PDF(pc) (6291KB)(98)       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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    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
    Abstract119)   HTML16)    PDF(pc) (10935KB)(173)       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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    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
    Abstract117)   HTML9)    PDF(pc) (12589KB)(129)       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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    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
    Abstract116)   HTML7)    PDF(pc) (7241KB)(109)       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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    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
    Abstract113)   HTML4)    PDF(pc) (5730KB)(112)       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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    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
    Abstract109)   HTML3)    PDF(pc) (7279KB)(148)       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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    Geochemical Characteristics of Cadmium, and Ecological Risk Assessment of Soil in Dongdagou Area,Baiyin City,Gansu Province
    HAN Baohua, DUAN Xingxing, HE Junlin, ADILAI Saitiniyazi, WANG Cuicui, DONG Yue
    Geoscience    2023, 37 (03): 745-757.   DOI: 10.19657/j.geoscience.1000-8527.2023.025
    Abstract108)   HTML4)    PDF(pc) (2147KB)(92)       Save

    Baiyin is an important non-ferrous metal province in China. Historically, unscientific and unreasonable mineral resource development and agricultural production activities have breached the heavy metal standards in Baiyin city and its surrounding areas. The controlling factors of bioavailability and ecological risk prediction of heavy metals have always been of great interest in biogeochemical behavior research. In this study, we investigated the contamination of root soil and corn seeds in/around the Dongdagou irrigation area (Baiyin city), analyzed the changes of key soil indicators in 2007 and 2018 in the local agricultural concentration area, and evaluated the ecological risks in the corn growing area. The local soil Cd content (average 17.48 mg/kg, maximum 51.1 mg/kg) exceeds the standard in some areas. The relative Cd content in different forms is carbonate state>ion exchange state>iron and manganese oxidation state>humic acid state>strong organic state>residue state≫water-soluble state. Factors such as high pH alkaline soil and low Cd accumulation of Cd-tolerant corn varieties limited the Cd bioavailability in the soil, and the exceedance rate of corn seeds is only 8.8%. There is certain Cd pollution in the local corn concentrated planting area, but it has been effectively controlled. Over half of the points of pH, Corg and CaO content that constrain the Cd bioavailability show an increasing trend, which imply that the risk will remain low for the coming future. To better control the areas with higher Cd content than the standard, we recommended to continue to choose low Cd accumulation of Cd-tolerant corn varieties for planting, and to harvest the seeds at maturity as animal feed or develop the corn seed resource industry. We also proposed to conduct recycling of other parts, especially the roots as restoration parts, to achieve reduction while restoration.

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    Discussion on Spot Size and Energy Density Effects on Zircon U-Pb Dating Precision
    HU Ziqi, ZHANG Dexian, LIU Lei
    Geoscience    2023, 37 (03): 722-732.   DOI: 10.19657/j.geoscience.1000-8527.2023.040
    Abstract107)   HTML2)    PDF(pc) (4858KB)(67)       Save

    LA-ICP-MS, an effective method for zircon U-Pb dating, is the most commonly used technology in geochronological studies. In the LA-ICP-MS zircon U-Pb dating process, the spot diameter and energy density are two important factors that can affect the dating precision. Zircon standard 91500 and GJ-1 are selected as both standards and unknown samples, respectively, and the effects of spot size and energy densities on the LA-ICP-MS U-Pb dating were determined. We aim to optimize the LA-ICP-MS zircon U-Pb dating method, improve the analysis accuracy, and provide reference for other laboratories to carry out similar research work. The results show that with fixed energy density when the ablation beam spot increases from 25 to 65 μm, the relative error (RE) between the measured age results and the recommended values of zircon 91500 and GJ-1 decreases continuously (RE=0.61%, 0.41%, 0.13%, and 0.08%, respectively), i.e., increasing the beam spot diameter can reduce RE and improve the dating precision. Under fixed beam spot diameter (35 μm) with energy density below or equal to 3.5 J/cm2, as the energy density increases, the relative error between the measured age results and the recommended values gradually decreases (RE=8.69%, 3.48%, 3.95%, 4.16%, and 0.41%, respectively), and the dating precision gradually increases. However, when the energy density is over 3.5 J/cm2, the energy density increase can lead to a significant increase in the denudation rate, and the fractionation effect in the depth direction increases greatly. The relative error between the measured ages and recommended values increases (RE=2.40% and 0.83%, respectively), and the dating precision decreases. Therefore, in the actual test, considering the sample size and the need to preserve the integrity of the sample, choosing reasonable energy density and beam spot size can effectively improve the dating precision.

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    Fluvial Geomorphology of the Eastern Altyn Tagh and Its Tectonic Activity Implications
    LU Fang, GAO Mingxing, ZHOU Shuxian, WANG Shun
    Geoscience    2023, 37 (05): 1100-1109.   DOI: 10.19657/j.geoscience.1000-8527.2023.020
    Abstract103)   HTML11)    PDF(pc) (8829KB)(248)       Save

    The Altyn Tagh strike-slip fault zone is the major control fault at the northern margin of the Qinghai-Tibet Plateau, and plays a vital role in the Cenozoic crustal deformation of the plateau.We extracted and calculated five geomorphic indices (slope, relief amplitude, fractal dimension, hypsometric integral, and stream length gradient) of 173 sub-basins by ArcGIS software.The geomorphic indices of each sub-basin were classified into five types.Their arithmetic mean values were used as relative tectonic activity indices, in order to quantitatively analyze the topographical features and the tectonic activity intensity.We show that Altyn Tagh strike-slip fault zone is the dividing line for the relative tectonic activity intensity of the whole study area, and the relative tectonic activity index level gradually decreases from south to north, and from high to low mountai-nous areas.From the spatial distribution of the relative activity tectonic index grade, the tectonic activity in the Danghe and Yemahe River basins appears to be stronger, and the intensity gradually decreases from west to east.In addition, we combine the influence of rocks, precipitation, and tectonics on the geomorphic index.Our results show that tectonics is the main factor controlling the geomorphic development in the watershed of the Altyn Tagh strike-slip fault zone, the relative tectonic activity intensity in the watershed where the seismic point is located, the watershed on both sides of the fracture zone, and the stress transition zone are higher than those in other surrounding watersheds.

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    Vegetation Dynamics and Driving Factors in Zhangjiakou-Chengde Area of Hebei Province from 2001 to 2020
    WANG Qian, JIN Xiaomei, ZHANG Xucai, YIN Xiulan, JIN Aifang, LUO Xufu
    Geoscience    2023, 37 (04): 881-891.   DOI: 10.19657/j.geoscience.1000-8527.2023.028
    Abstract101)   HTML5)    PDF(pc) (8786KB)(140)       Save

    As a water conservation function area in the Beijing-Tianjin-Hebei region, the vegetation dynamics of Zhangjiakou-Chengde (Zhang-Cheng) area is of great significance for the ecological/environmental construction and protection. Based on MODIS-NDVI, temperature and precipitation, land use, groundwater depth and measured soil moisture data, Sen+Mann-Kendall trend analysis, partial correlation analysis and other methods, we analyze the spatial-temporal variation characteristics of vegetation and the response characteristics of temperature and precipitation, land use, groundwater depth and soil moisture in Zhang-Cheng area from 2001 to 2020. The results show that the annual mean NDVI value shows an upward fluctuation trend. The vegetation coverage is characterized by being low in the northwest and high in the southeast. Significant vegetation improvement areas were mainly distributed across most of Baxia, accounting for 85.79% of the study area. There are positive correlations between precipitation, temperature, and the vegetation index. Furthermore, the vegetation variation agrees well with the land-use change. The vegetation growth is best when the groundwater depth is around 6.2 m. The spatial distribution of soil moisture is low at Bashang and high at Baxia. The NDVI increases with increasing measured soil moisture.

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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
    Abstract100)   HTML19)    PDF(pc) (7090KB)(133)       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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    Middle Late-Pleistocene Sporopollen Records of Ake River III Terrace in Southern Margin of Aba Basin, Western Sichuan
    ZHU Ting, HE Zhengwei, YANG Zhenjing, KANG Guichuan, GUAN Sensen, ZHU Yuting
    Geoscience    2023, 37 (04): 870-880.   DOI: 10.19657/j.geoscience.1000-8527.2022.037
    Abstract98)   HTML7)    PDF(pc) (6369KB)(129)       Save

    Vegetation growth and change have important implications for climatic evolution. In this study, we used sporopollen record to reconstruct paleovegetation and paleoclimate. Based on the sporopollen study of the Ake River III-level terrace in the southern margin of Aba basin in western Sichuan (eastern Qinghai-Tibet Pla-teau)and OSL dating, the results show that PM01 is (78.4±7.1) to (71.6±6.2) ka B.P. (middle Late Pleistocene). According to the palynological assemblage and mathematical analysis, the PM01 profile was divi-ded into three palynological zones. The results show that vegetation in the Aba Basin was sparse forest and grassland from (78.4±7.1) to (71.6±6.2) ka B.P. in the middle Late Pleistocene. The paleoclimate evolution can be divided into three stages: (1) cold and arid; (2)warmer than the first stage, but still cold and dry; (3)warmer and then cooler and drier. The results are consistent with the climate evolution trend of the last ice age, and provide new data for the study of the Quaternary regional vegetation and climate evolution, which is of great significance for studying Quaternary paleoclimate in the eastern Qinghai-Tibetan Plateau.

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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
    Abstract98)   HTML15)    PDF(pc) (16110KB)(194)       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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    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
    Abstract97)   HTML6)    PDF(pc) (31168KB)(124)       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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    Value and Excavation of Geological Culture: Taking Ahetan Geological Culture Village in Hualong County, Qinghai Province as An Example
    WANG Yifan, ZHANG Xujiao, ZHANG Xiangge, LI Junlei, YUAN Xiaoning, WANG Kaiya, LIU Xinlan, WANG Chongge, RAO Haoshu, LIU Jiang, QIN Yuan
    Geoscience    2023, 37 (05): 1423-1434.   DOI: 10.19657/j.geoscience.1000-8527.2023.114
    Abstract97)   HTML7)    PDF(pc) (16575KB)(168)       Save

    The construction of geological culture villages is in full swing across the country. However, its theoretical basis is not very clear, and especially most villages’ geological culture has not been fully excavated and demonstrated. Therefore, the excavation of geological culture becomes an urgent problem to be solved in the construction of geological culture villages. In 2022, Ahetan Geological Culture Village was awarded the first three-star geological culture villages in Yellow River Basin and Qinghai Province. It has made beneficial attempts and obtained good effects on geological culture excavation and three-dimensional expansion of rural culture revitalization. Based on the investigation and evaluation of heritages in Ahetan, including Yellow River terraces, ancient springs, ancient city, hollow elm tree, etc., and the in-depth excavation of geological culture, this paper systematically summarizes the definition, value, and excavation method of geological culture, and proposes it should be the theoretical basis of the construction of geological culture villages. Geological culture is all the material and spiritual wealth formed by human beings in the process of understanding, adapting, utilizing, and reforming the earth. The excavation of geological culture should focus on the close connection between geological processes and human civilization, reconstructing the history of geological processes and the harmonious relationship between humans and the planet, and demonstrating it to the public by commentary system. Through systematic summarization of geological culture and its excavation method, this paper aims to provide references for the construction and development of geological culture villages across the country.

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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
    Abstract95)   HTML8)    PDF(pc) (9825KB)(94)       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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    Geochemical Characteristics of Stream Sediments and Prospecting in the Middle Reach of the Nalinggele River, Qinghai Province
    ZHANG Wei, AN Maoguo, WANG Zhipeng, YANG Qi, CHEN Huaixin, MA Xiaofeng, ZHI Chenglong, XING Qitao, PEI Changshi, WANG Na, LIU Ming
    Geoscience    2023, 37 (03): 690-707.   DOI: 10.19657/j.geoscience.1000-8527.2022.042
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    The middle reach of the Nalinggele River in Qinghai Province is located in the Qin-Qi-Kun ore domain and the Variscan Qimantag Dulan Fe-Co-Cu-Pb-Zn-Sn-W ore belt in the eastern Kunlun mineral province. Over ten metal deposits/prospects have been discovered in/around this area, with good prospects for gold, iron, lead, zinc, copper, and nickel exploration. This study is based on the new 20-element analysis on stream sediment samples, and statistical analysis of element distribution and characteristic parameters to summarize the enrichment and dispersion regularities, element assemblage characteristics, and their relationship with metallogenic conditions. The results show that Pb, Bi, and Zn are significantly enriched in the Baishahe Formation, with a high mineralization index. Cu, Cr, Ni, Co, and V are significantly enriched in the Tanjianshan Group. The high-temperature Indosinian felsic magmatic activity could provide sufficient heat for the metal remobilization (e.g., Cu, Pb, Zn)in the formation. The skarn belt formed by contact metamorphism and metasomatism between the strata and the Indosinian felsic magma represents a favorable site for skarn-type Cu, Pb, Zn polymetallic mineral exploration. In combination with the geological conditions and geochemical characteristics of mineralization, a total of 39 geochemical comprehensive anomalies have been delineated, and 5 prospects have been defined. Among them, the Yemaquan-Niukutou-Heishan Cu-Au-Sb and the Ketihar-Hongweishan Cu-Co-Ni-V polymetallic prospects can be regarded as the key Cu polymetallic metallogenic prospect zone in the region with relatively high metallogenic potential. This study provides a reference for the optimization of multiple non-ferrous metal mineral target areas in the region, resource potential evaluation, and further geological exploration work.

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    Petrogenesis and Tectonic Significance of the Late Triassic Nanmulin Intermediate-felsic Magmatic Rocks in the Gangdese Batholith, Southern Tibet
    HAN Fei, SONG Yuanbao, ZHANG Wei, LI Daoling, HUANG Yonggao, LI Yingxu, JIA Xiaochuan, YANG Xuejun, YANG Qingsong, SONG Xubo, LU Liu
    Geoscience    2023, 37 (03): 547-561.   DOI: 10.19657/j.geoscience.1000-8527.2023.011
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    The initial Neo-Tethyan evolution in the Lhasa block is an important part for the reconstruction of the Tethys space-time framework. Due to the lack of research objective, its understanding needs to be deepened. The Nanmulin granodiorite and quartz diorite are located in the central Lhasa block. We conducted systematic zircon LA-ICP-MS U-Pb dating and whole-rock geochemical analyses for determining the petrogenesis and source region of these rocks. The results provide new constraints for the early Neo-Tethyan evolution. Zircon U-Pb dating shows that both lithologies were formed in the Late Triassic, with the granodiorite emplaced at (214.3±1.1) Ma and the quartz diorite at (206.1±1.3) Ma. Geochemically, these rocks have Rittmann index (σ) of 1.79-4.71 and are calc-alkaline. They are peraluminous with Al2O3 varying from 15.01% to 17.57%,and A/CNK=0.76-1.12. Moreover, the granodiorite has high SiO2(61.87%-73.72%, average 65.76%) and high K (up to 4.25%) and low Mg#(31-46, average 41). Rb, U, K, Pb and LREEs are enriched and Nb, Ta, Ti and HREEs are depleted, suggesting arc-related or crust-like geochemical affinities. Rb/Sr (0.05-5.50, average 2.54) values suggest that their parental magmas were crustal sourced. The granodiorite and quartz diorite have high (La/Yb)N values (average 12.05), with no clearly negative Eu anomalies (δEu=0.57-1.01, average 0.73). In summary, these data indicate that the Nanmulin intermediate-felsic rocks are I-type formed by the partial melting of juvenile crust. We propose that the northward subduction of the Neo-Tethyan was initiated before Late Triassic, which was before the formation of the newly-discovered Late Triassic Be-RB±(Nb-Ta) rare metal mineralization.

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    Geochronology and Geochemistry of the Intermediate-basic Dikes in the Beishan Area, Inner Mongolia: Implications for Tectonic Evolution of the Northern Margin of the Tarim Plate
    XUE Zhongkai, FAN Baocheng, HUANG Haoqing, TANG Weidong, GE Zhanlin, LI Pengwei, HU Jianhui, YANG Xiaoqi, GUO Yongchao, LI Kong
    Geoscience    2023, 37 (03): 627-644.   DOI: 10.19657/j.geoscience.1000-8527.2022.089
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    The formation age and genesis of the altered intermediate bedrock dike in the Laodonggou gold depo-sit (Ejin Banner, northern margin of Tarim terrane) provide a window to study the gold mineralization constraints and the Paleo-Asian Ocean evolution. In this study, a series of gold ore-related diabase dike and altered diorite porphyrite dike samples were collected from the Laodonggou ore section II, on which we conducted LA-ICP-MS zircon U-Pb dating, Hf isotope and whole-rock geochemical analyses. The results showed that the emplacement of diabase dikes and diorite porphyrite dikes occurred in the Early Permian (286.5±1.7 Ma) and Middle Triassic (243.2±1.1 Ma), respectively, and such age sequence is consistent with the observed field crosscutting relationship. According to the characteristics of diorite porphyrite dikes interlaced with gold orebo-dies, the gold mineralization is suggested to be slightly after 243 Ma. Zircon εHf(t) value of the diabase dikes ranges from -3.67 to 0.97, and the whole-rock element composition shows that the rocks are peraluminous calc-alkaline. This indicates that the magma source region contains both Neoproterozoic juvenile crustal components and Mesoproterozoic ancient crustal components. Altered diorite porphyrite dike εHf(t)=-0.07 to -4.76, and the whole-rock element composition is the peraluminous K-rich basalt series (K-rich characteristics affected by the potassic alteration in the mining area), indicating that the magma is mainly derived from the Mesoproterozoic crustal melting. Based on the Late Paleozoic to Early Mesozoic tectonic evolution in the northern margin of the Tarim block, we proposed that the Late Carboniferous-Early Permian paleo-oceanic basin subduction in the Beishan region may have led to partial melting of the mantle wedge, and that the magma may have ascended into shallow faults and cooled to form diabase dikes. In the end Early Permian, the Beishan region entered an intracontinental tectonic stage, and post-orogenic extension occurred in the Middle Triassic. This likely resulted in the decompression and melting of Mesoproterozoic crustal materials, and magma emplacement along crustal faults to form diorite porphyrite dikes.

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    Enrichment Mechanism of Deep Groundwater with High Fluoride in Coastal Plains: A Case Study of the Luanhe Delta
    ZHANG Zhuo, CHEN Sheming, LIU Futian, GAO Zhipeng, NIU Xiaotong
    Geoscience    2023, 37 (04): 925-932.   DOI: 10.19657/j.geoscience.1000-8527.2022.029
    Abstract92)   HTML5)    PDF(pc) (9280KB)(107)       Save

    High F- groundwater has been found in deep aquifers of the coastal plain region, which seriously threatens the domestic water safety. To ascertain its enrichment mechanism, sixty-nine groundwater samples on site were collected for hydrochemical and isotopic analyses of the low- and high-fluoride groundwater. The results show that high fluoride groundwater mainly exists in Na-HCO3-type groundwater, while the chemical type of low-fluoride groundwater is mainly Ca·Na-HCO3. Saturation index calculation shows that the groundwater samples are mostly fluorite undersaturated but calcite oversaturated. This indicates that fluorite dissolution is favored with precipitations of Ca2+ as calcite, thus leading to higher F- level in the groundwater. The linear regression results show that cation exchange occurred between Ca2+ and Na+ in deep groundwater, which could decrease the groundwater Ca2+ content and further promote the CaF2 dissolution. There is good positive correlations between F- and pH and HCO 3 - in deep groundwater, indicating that the slightly alkaline environment and high HCO 3 - content are beneficial to F- desorption. In addition, there is strong positive F- vs. Li correlation in deep groundwater, which also indicates that the local mixing of geothermal water may directly affect the F- enrichment in deep groundwater. Comparing the hydrochemical and isotopic characteristics of deep groundwater with seawater, we found that the local F- enrichment of deep groundwater is unaffected by seawater intrusion.

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    Route Planning and Ponder of Geoscience Study Travel in Hualong County, Qinghai Province
    LI Junlei, ZHANG Xujiao, WANG Yifan, ZHANG Xiangge, WANG Chongge, YUAN Xiaoning, LIU Xinlan, WANG Kaiya, RAO Haoshu, LIU Jiang, QIN Yuan
    Geoscience    2023, 37 (05): 1411-1422.   DOI: 10.19657/j.geoscience.1000-8527.2023.113
    Abstract92)   HTML11)    PDF(pc) (12118KB)(230)       Save

    Geoscience study travel is a new engine to utilize the resources of geological heritage to carry out the popularization of geoscience, which in turn leads to geotourism. Yet, due to the fact that the guiding ideology and methodology of study route planning are still unclear, there are problems such as limited study objects, superficial course contents, insufficient scientific inquiry, and emphasizing on touring but not on studying, etc. in geoscience study in general. Hualong County in Qinghai Province, which is located in the upper reaches of the Yellow River, preserving significant geological heritage such as the convergence of Rodinia supercontinent, the subduction and closure of the Proto-Tethys Ocean, the uplift of the Tibetan Plateau and the Yellow River evolution, etc., which is a unique resource to carry out geoscience study travel. This paper discusses the design ideas of geoscience study planning from the guiding ideology, scientific questions and supporting facilities, taking Huarong County as an example.Based on the detailed field geological survey, the characteristics, types, distribution and scientific value of geological heritage in Hualong County have been systematically researched and deeply excavated. Taking the Early Paleozoic Ophiolite Suite in Laji Mountain, Xining Group-Hualong Complex Angular Unconformity, Danxia landform, Red Soil Forest landform and paleoseismic dammed-lake as the key points of the study, we have planned out the Lamu Gorge-Heshijia “the Meeting of one Billion Years”, Ahetan Village-Gongbo Gorge “Flowing Water-the Sculptor of Nature”, Keba Village-Jinyuan Township “Double-edged Sword of Neotectonic Movement”, Yaoshuiquan-Ansiduo Township “Conversion of Sea and Land with Ophiolite”, Xiaqiong Temple-Gangshan Mountain “the Winding Yellow River, the Forest Sea of Plateau”, a total of five geoscience study routes. It also proposes the methods of planning and designing geoscience study routes oriented by geoscience questions and guided by the earth system view and the theory of harmonious coexistence between man and nature. It can provide a scientific basis for the development of geotourism in Hualong County, and also has a certain reference value for the development of geoscience study in other areas.

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    Organic Nano-pore Textural Characteristics of the Longmaxi Formation Shale in the Southeastern Sichuan Basin
    LI Dongsheng, GAO Ping, GAI Haifeng, LIU Ruobing, CAI Yidong, LI Gang, ZHOU Qin, XIAO Xianming
    Geoscience    2023, 37 (05): 1293-1305.   DOI: 10.19657/j.geoscience.1000-8527.2023.054
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    The widely developed nano-pores in organic-rich shale are important storage space for shale gas.To determine the pore development characteristics of organic matter in shale, the Lower Silurian Longmaxi Formation shale in Dingshan area, southeast Sichuan Basin is taken as the research object.The surface porosity of organic matter was evaluated and the nano-pore structure characteristics were characterized based on scanning electron microscopy (SEM) and low-pressure N2 and CO2 adsorption analysis.The results indicate that total organic carbon (TOC) content was the major factor influencing the specific surface area and pore volume of nanopores in the Longmaxi Formation shale.With increasing TOC contents, the specific surface area and volume of organic pores increase.With higher TOC contents, the specific surface area and volume of organic pores played a dominant role over that of inorganic pores.The pore volume contribution of the 2-10 nm-sized pores to the total pore volume is the largest in the Longmaxi shale samples, and the pyrobitumen contains larger numbers of mesopores than the other types of organic matter (e.g., kerogen).The pyrobitumen content increase would significantly increase the mesopore volumes of the shale.However, the oil expulsion efficiency can indirectly affect the nanopore development via the variation of pyrobitumen contents.The volume of mesopores and total pores in the shale would be reduced due to high oil expulsion efficiency.In the exploration and development of Longmaxi Formation shale, the influence of TOC content, oil expulsion efficiency and pyrobitumen content on the reservoir conditions of shale gas should be considered comprehensively.

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    Development Characteristics and Risk Assessment of the Damogou Debris Flow in Mentougou District, Beijing
    NIE Qiong, NIE Zhibao, CHEN Jian, DING Shijun, WU Saier, LI Duo, GE Runze, CHEN Ruichen
    Geoscience    2023, 37 (04): 1013-1022.   DOI: 10.19657/j.geoscience.1000-8527.2022.086
    Abstract87)   HTML6)    PDF(pc) (9902KB)(97)       Save

    Debris flow is one of the most common types of geological disasters in western and northern Beijing mountainous areas during stormy seasons. In the history of Damogou Gully (Qingshui town, Mentougou district, Beijing), there were many periods of debris flow disasters. At present, there are still many artificial deposits and collapse accumulations that constitute a potential debris flow source, and there are serious debris flow hidden dangers. This study identifies the types of debris flow sources, their storage and distribution, simulates the debris flow impact range under the frequency of once every 10, 20, 50 and 100 year rainfall, and evaluates their respective risk. The results show that the potential debris flow source is mainly man-made waste slag and coal gangue, with the residual reserve of ~447,000 m3. The high-risk debris flow area accounts for 13.1%-20.0%, mainly distributed in the gully mouth accumulation area and the confluence of main and branch gullies. The proportion of medium-risk area is 29.9%-31.2%, and the proportion of low-risk area is 48.8%-57.0%. It is advisable to set up prevention and control measures of upstream interception and downstream drainage in the circulation area of Damogou gully, and strengthen the rainfall monitoring and warning in the formation area in the heavy rainfall seasons.

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    Ecological Vulnerability Evaluation and Countermeasures of Ecological Restoration in Ecological Restoration Areas of Mountains-Rivers-Forests-Farmlands-Lakes-Grasslands,Tai’an City
    XU Fei, JIAO Yuguo, TANG Liwei, WEI Kai, YIN Yanpeng, HU Qingling, ZHAI Daiting, ZHAO Xinchu
    Geoscience    2023, 37 (04): 892-902.   DOI: 10.19657/j.geoscience.1000-8527.2021.152
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    Ecological protection and restoration has become a core content for the construction of ecological civilization in China. The study of ecological vulnerability is an important basis for evaluating ecological environmental problems, and for performing ecological protection and restoration. To scientifically identify the formation mechanism and ecosystem vulnerability variation in the ecological restoration area of mountains-rivers-forests-farmlands-lakes-grasslands in Tai’an City, and to clarify the direction of ecological protection and restoration, we used the pressure state response (PSR) framework model to evaluate the local ecological vulnerability. We further diagnosed the ecological environment problems in combination with the evaluation results, thus put forward countermeasures for ecological protection and restoration. The results show that the low vulnerability areas account for the highest proportion (37.97%), indicating that the overall local ecosystem is relatively stable. Among the investigated counties, cities and districts, there is higher proportion of vulnerability areas in the Taishan (48.77%) and Daiyue (37.15%) districts and Feicheng (30.97%) city, indicating that the ecosystem of the three counties is unstable. Considering the local situation, we put forward five ecological restoration suggestions, including (1) promote mine ecological restoration, (2) improve forest and grass coverage, (3) comprehensively regulate the watershed system, (4) increase biodiversity and improve ecological security system. The evaluation results and the proposed ecological restoration countermeasures are helpful to the rational layout of the project. It can also facilitate the targeted planning of the construction of ecological civilization in the implementation of the local ecological protection and restoration project of mountains-rivers-forests-farmlands-lakes-grasslands, and provide reference for the implementation of the ecological restoration project of mountains-rivers-forests-farmlands-lakes-grasslands in China.

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    Impacts of Cadmium Concentration in Rhizospheric Soil of Corn on Bacterial Communities: A Case Study from Silong Town, Baiyin City, Gansu Province
    HU Yonghao, DUAN Xingxing, XIA Zhaode, HAN Baohua
    Geoscience    2023, 37 (03): 758-766.   DOI: 10.19657/j.geoscience.1000-8527.2023.029
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    To explore the response of bacterial communities of corn in rhizospheric soil to Cd pollution, we utilized the Illumina MiSeq high throughput sequencing platform, and conducted 16S rDNA amplification analysis on four groups of soil samples with different levels of Cd pollution from Silong Town (Baiyin City, Gansu Pro-vince). The results showed no significant difference in the Chao1 and Shannon indices of soil bacterial samples from these four groups of Cd-polluted samples (p>0.05), indicating that the pollution effect is insignificant. The bacterial abundance of the four sample groups is similar, and the dominant communities are largely the same, i.e., (phylum level) Proteobacteria, Bacteroidetes, Acidobacteria, Chloroflexi and Planctomycetes, and (dominant genera) are Ohtaekwangia, GP4, GP6, Nitrospira and Gemmatimonas. The Ohtaekwangia and Gemmatimonas have high stress resistance, and their relative abundance increases with increasing soil Cd content. In contrast, GP4 and GP6 have low stress resistance, and their relative abundance decreases with decreasing soil Cd content. Cadmium pollution can cause changes in bacterial diversity in the soil, but there is no simple linear relationship between bacterial diversity and Cd content. With increasing Cd content in the environment, soil bacterial diversity generally increases first and then decreases. Soil samples with intermediate pollution level have the highest bacterial diversity.

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