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    10 October 2017, Volume 31 Issue 05
    Research on the Main Geohazards and Engineering Geological Problems Along the SichuanTibet Railway
    Discussion on the Environmental and Engineering Geological Problems Along the Sichuan-Tibet Railway and Its Adjacent Area
    GUO Changbao, ZHANG Yongshuang, JIANG Liangwen, SHI Jusong, MENG Wen, DU Yuben, MA Chuntian
    2017, 31(05):  877-889. 
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    The Sichuan-Tibet Railway is one of the most important main railway lines under planned and construction of China, and it is an important part of China western transportation system. However, because the railway passes through several big tectonic units, e.g. the Yangtze plate, Sichuan-Yunnan plate, Qiangtang plate and Lhasa plate, under these complex geological conditions, there are some complex geological problems along the Sichuan-Tibet Railway, such as active faults, earthquakes and other geohazards, and thus the planning and construction of the Sichuan-Tibet Railway are restricted. Based on the field geological investigation, geological drilling, analysis of in-situ stress measurements and laboratory testing, the paper analyzes the main environmental and engineering geological problems along the railway, e.g. active faults, high crustal stress, high geothermal activities, rock burst and geodisasters that might occur in the process of railway construction. And the authors deem that there are 54 regional active faults along the Sichuan-Tibet Railway and its adjacent area, and 17 of them are active faults and have directly important effect on the railway construction; the earthquake is frequent in the study area, and 50% of the planning route is located in the area of seismic peak ground acceleration more than 0.2 g, part of the region more than 0.4 g,so the potential seismic risk is likely to happen; the main geohazards are collapse, landslide and debris flow along the railway, most of them are controlled and affected by active faults, and the long run-out landslides are also developed in this area; the tectonic stress and geothermal field are complicated along the railway, and some serious engineering problems are in high risk in the railway construction, such as rock burst, soft rock’s big deformation, and high geothermal calamity.

    Discovery and Significance of the Lacustrine Sedimentation in the Middle Reach of Yarlung Zangbo River in Tibetan Plateau
    HAN Jian’en, MENG Qingwei, GUO Changbao, SHAO Zhaogang, WANG Jin, YU Jia, XU Biao
    2017, 31(05):  890-899. 
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    The authors recognized a barrier lake in the middle reach of the Yarlung Zangbo River, which is formed by the glacier blocking the river during the late stage of Late Pleistocene. The field investigation finds that the lacustrine strata are in the Sangri County, Nêdong County, Zhanang County and other places along the middle reach of Yarlung Zangbo River, showing that the lake is a large paleaolake with an area of more than 700 km2 from Zaba village near Sangri County (east) to Gonggar airport (west), i.e.the Jiedexiu paleaolake. The lacustrine sedimentary section is typically a continuous silty clay layer and has horizontal bedding structures; the thickness of the section in Jiedexiu town of Gonggar County is the largest and more than 10 meters; the AMS 14C age of the top of the section is 15,680-15,105 aBP, belonging to the Last Glacial Maximum (LGM) period. Combined with the formation age and sedimentary characteristics of the lacustrine strata in Linzhi, Songzong, Gega paleaolake and other areas along the lower reach of the Yarlung Zangbo River, the results reveal that the Jiedexiu paleaolake develops during the LGM period; the characteristics of sediments and storage capacity of paleaolake show that the Jiedexiu paleaolake is not completely blocked during developing period, but a large-scale lake of taking in and sending out waters, liking a modern reservoir. The spatial characteristics of moraine, which is found in the south bank of the Yarlung Zangbo River, and lacustrine sediments in the board valley of the river, indicate that the Jiedexiu paleaolake is formed from glaciers blocking the Yarlung Zangbo River during the LGM period. This paper also demonstrates that the Yarlung Zangbo River is an antecedent river, it isn’t formed by headwater erosion of many paleaolake in the region, but it exists there before the formation of the Jiedexiu and other paleaolakes. Paleaolakes, such as Jiedexiu paleaolake in the Yarlung Zangbo River basin, are formed by blocking river valley caused by climate changes, neotectonic movement, and seismic activity and so on.

    Analysis of In-situ Stress Measurement and Real-time Monitoring Results in Nyching of Tibetan Plateau and Its Response to Nepal MS8.1 Earthquake
    ZHANG Peng, QU Yaming, GUO Changbao, FENG Chengjun, MENG Wen, FAN Yulu, TAN Chengxuan, WANG Lei
    2017, 31(05):  900-910. 
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    To explore the in-situ stress in the fracture belt and its present activity, the authors gathered data from hydraulic fracturing for in-situ stress measurement and from piezomagnetic method for monitoring relative magnitude of in-situ stress along the drilling hole with total depth of 300 meters located in a granite-rich region in the northern part of Nyching, Tibet. The measurements of in-situ stress indicate the relationship of SH>Sh≥SV, and the structure features of shallow earth’s crust rock formation reveal that current horizontal principal stresses play a leading role in reverse fault activity. Moreover, the measured maximum principal in-situ stress strikes in NNE direction, reflecting present compressive properties with dextral slip activity of faulting to north-east and near-south-north trend. Calculated through measured principal stresses, the magnitudes of feature parameters (μm) are obtained to be in the range of 0.11 to 0.23, which reflect a lower-stress accumulative capability of the regional crust and inactivity of fault movement in this area. Although the direction of the maximum horizontal principal stress remains basically unchanged in the occurrence of Nepal MS8.1 earthquake, the stress-monitoring results show that before the earthquake the values of the maximum and minimum horizontal principal stresses increase in 0.35 MPa and 0.24 MPa, respectively; during the earthquake for the co-seismic effect the reduced values are 0.05 MPa and 0.04 MPa, respectively; while four months later after the earthquake the maximum horizontal principal stress is reduced by 0.05 MPa, and the minimum principal stress increases by 0.01 MPa. Based on the in-situ stress measuring and real-time monitoring results while the earthquakes happen, the change of stress fields can be investigated to understand the activity of regional faults and it is much significant for the study of seismic risk and crustal stability.

    Geohazard Susceptibility Assessment Along the Sichuan-Tibet Railway and Its Adjacent Area Using an Improved Frequency Ratio Method
    LI Langping, LAN Hengxing, GUO Changbao, ZHANG Yongshuang, LI Quanwen, WU Yuming
    2017, 31(05):  911-929. 
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    The Sichuan-Tibet Railway (STR) is one of the most important main railway lines under construction of China. However, the STR is located in the east of the Tibetan Plateau, which is characterized by complex topography and geology. The complex geological backgrounds and fragile geological environments make geohazards highly develop along the STR and its adjacent area, which in turn threat the construction and operation of the STR. This paper firstly developed an improved frequency ratio method for geohazard susceptibility assessment, which overcomes the discontinuity of frequency ratio values faced by the traditional frequency ratio method, and increases the capability of distinguishing geohazard sensitivity of influencing factors, and also reduces the subjectivity during the classification of influencing factors. The merit of the improved method compared with the traditional method was verified by quantitative analysis on geohazard susceptibility models using ROC curve and spatial entropy. According to the developing and spatial distribution characteristics of geohazards, this paper chose topographic elevation, topographic slope, topographic aspect, topographic curvature, topographic relief, engineering geological strata, peak ground acceleration, density of faults, distance to rivers, distance to roads, precipitation and vegetation index as the fundamental influencing factors of geohazards. The geohazard susceptibility assessment and zonation along the STR and its adjacent area were implemented based on the improved frequency ratio method and historical geohazard data. The results showed that, the spatial distribution of the geohazard susceptibility along the STR and its adjacent area is mainly constrained by the spatial distribution of those linear features such as faults, waters and roads as well as the spatial distribution of topographic factors such as topographic slope and topographic relief, while density of faults and topographic relief are two factors with the highest capabilities of distinguishing geohazard sensitivity. The extreme high and high geohazard susceptibility zones are mainly located along the major rivers and roads in the research area. Since the railway lines are mainly distributed along rivers and existed roads, those zones should be paid particular attention during the construction and operation stages of the railway regarding the monitoring and prevention of geohazards.

    Remote Sensing Interpretation of Large Landslides Along Sichuan-Tibet Railway Based on Object-oriented Classification Method
    SU Fangrui, GUO Changbao, ZHANG Xueke, SHEN Wei, LIU Xiaoyi, REN Sanshao
    2017, 31(05):  930-942. 
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    The Sichuan-Tibet Railway is located in the Middle and East of the Tibetan Plateau, where the landforms and geological structures are very complicated. The large scale landslides are densely developed in this area, and they have caused serious human life casualties and losses of major projects. Based on the zonal remote sensing image data, taking the example of Chashushan landslide, 102 Daoban landslide, Nujiang landslide and Luanshibao landslide along the Sichuan-Tibet Railway, this study takes the method of object-oriented classification to analyze the remote sensing information of landslides by use of high resolution WorldView-2 and Landsat TM remote sensing image data on the ENVI5.1 and eCognition software platforms. The result shows that the key information and target area can be extracted by object-oriented classification method, and combined with visual interpretation the details of landslides can be obtained, which can improve the success rate of landslide interpretation. It is of great significance to the landslide survey in the complicated geological conditions along Sichuan-Tibet Railway. Finally, this study combined the grey-level co-occurrence matrix (GLCM) and normalized difference vegetation index (NDVI) to discuss the identification of the ancient landslide and the reactive landslide, and on this basis supposed to put forward the GVI model and constructed the mass function IGVI of GVI model. The results of statistical samples show that the IGVI value of the ancient landslide is lower than that of the reactive landslide, indicating that the GVI model proposed in this paper can provide a basis for identifying the ancient landslide and the reactive landslide.

    Research on the Weakening Mechanism of the Mechanical Behavior for the Granite in the Eastern Qinghai-Tibet Plateau Under the Condition of Freezing-Thawing Cycles
    GUO Changbao, ZHOU Jiazuo, LIU Xiaoyi, REN Sanshao, WU Rui’an
    2017, 31(05):  943-955. 
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    The granite in the eastern Qinghai-Tibet Plateau was tested by the freezing-thawing-cyclic testing, and the damage trend of rock during freezing and thawing was analyzed by the wave velocity testing and nuclear magnetic resonance (NMR). The testing results showed that as the number of freezing-thawing cycles increased, the inner damage degree increased and the wave velocity decreased obviously. The T2 distribution and development of NMR implied that the range of the size of cracks in the more weathered rock samples became wider due to freezing-thawing cycles, while the size of the cracks in the less weathered samples is more concentrative. The samples which were tested by freezing and thawing were then tested on triaxial testing apparatus. The testing results showed that the uniaxial compressive strength and the elastic modulus decreased as the number of freezing-thawing cycles increased, but the Poisson’s ratio and internal friction angle varied randomly. Based on the testing data and theoretical analysis, a freezing-thawing-damage constitutive model was presented, which can be used for simulating and predicting the overall variation of stress and strain of rocks.

    Research on Geohazard Developing Characteristics in Jiacha to Langxian Section of Sichuan-Tibet Railway
    WU Rui’an, GUO Changbao, DU Yuben, WANG Ke, DU Guoliang
    2017, 31(05):  956-964. 
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    The Jiacha to Langxian section of the Sichuan-Tibet Railway is located in the middle reach of the Yarlung Zangbo river in the southeast of the Tibetan plateau. It is one of the regions in China suffering from serious geological hazards, where topography is complex; tectonic activities are intense as well as high density geohazards develop in this area. On the basis of data collection and remote sensing, this study made a survey of geohazards in Jiacha to Langxian section of the Sichuan-Tibet Railway and investigated 139 geohazard spots including landslides, collapses and mudslides five kilometers from railway on both sides in an area of 780 km2. This study also discovered a high-speed and long-runout landslide in Lagangcun and Ri’amo large landslide along the Yarlung Zangbo river. The geohazard developing characteristics and formation mechanism are analyzed in this paper. Research results show that Yarlung Zangbo fault has definite control action on the morphology and rock mass structure, resulting in landslides and collapses zonally distributed along the fault, and that is one of the main geohazard developing characteristics in the study area, and the sliding directions of about 53% of collapses and landslides are perpendicular to the strike of the Yarlung Zangbo fault, while about 30% are parallel to the fault. Under the influence of rapid uplift of the crust and river erosion, developing characteristics of geohazards have remarkable differences between open valley and canyon along Yarlung Zangbo river. Fault activities, especially earthquakes induced by the violent activities of faults offer geological background for high-speed and long-runout landslides, i.e.high-speed and long-runout landslide in Lagang. The coupling effects of endogenic and exogenic process, containing fault activities, rainfall and engineering activities, make the formation mechanism of geohazards more complex, and some landslides in bad stability can be reactive repeatedly, imposing a negative influence on planning construction of major projects, and the prevention and reduction of geohazards.

    Study of Slow-moving Landslide Characteristics Based on the SBAS-InSAR in the Xianshuihe Fault Zone
    LIU Xiaoyi, YANG Zhihua, GUO Changbao, SHEN Wei, SU Fangrui
    2017, 31(05):  965-977. 
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    Xianshuihe Fault is one of the most important boundary fault on the eastern Tibetan Plateau of Sichuan-Yunnan block, and it is strongly active since the Holocene. The rock-mass and soil-body structures are porous along the Xianshuihe Fault zone. Under the action of earthquake caused by the active fault and its slowly moving and heavy rainfalls, landslides and debris flows occur frequently and have caused serious harm in this area. On the basis of the previous studies, SBAS-InSAR (small baseline subset interferometric synthetic aperture radar) method is employed to analyze and calculate the activity rate of Daofu to Luhuo section in Xianshuihe Fault zone combined with fifteen PALSAR scene data acquired by ALOS-1 during 2007-2011. And the deformation characteristics of time series are also acquired about the creeping landslide occurring along Xianshuihe Fault in these five years. The results show that in recent years the creeping in Daofu to Luhuo section is the mainly active type for the fault, and the creeping rate is about (9.4±0.78) mm/a, and the creeping effect of the fault has an important influence on the occurrence of landslides in this area. While the distance from Xianshuihe Fault is closer, the coherence among images is stronger, and coherent points are more stable and the interference effect is better, thus the cumulative displacement of landslides is greater. Ninety-eight creeping landslides along Daofu to Luhuo section of Xianshuihe Fault are identified, linearly distributing along both sides of the fault; the surface deformation characteristics of the typical creep landslide is also analyzed. Based on SBAS-InSAR Radar Data Processing method, we can effectively analyze the slow deformation of the surface, and the changing and developing laws of these regional creeping landslides. This study plays a certain guiding role on the prevention and mitigation of geohazards along Xianshuihe Fault and in the other similar areas.

    Development Characteristics and Formation Mechanism of Chashushan Landslide in Batang, Western Sichuan
    REN Sanshao, GUO Changbao, ZHANG Yongshuang, ZHOU Nengjuan, DU Guoliang
    2017, 31(05):  978-989. 
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    Chashushan landslide is located in the intersection of Batang fault and Jinshajiang fault. With the complex geological structure and intense neotectonic movement, large landslides occur frequently in this area. Chashushan landslide originates from ancient landslide mass. The sliding deformation of the landslide first appeared in July of 2001, followed by creep deformation. Deformation velocity of the landslide was accelerating continuously because of deformation. Then a lot of distortion evidences appeared in the landslide mass. Finally, the landslide occured severely sliding on January 7,2006. The landslide is in unstable condition, and the deformation and failure of the landslide are obvious, and it is potential that the deformation and failure will last. Through field investigation, large-scale direct shear tests on slipping soils were carried out, then the shear strength was obtained under the condition of different water contents, which revealed the cohesion and internal friction angle decreased with the increase of water content. In this paper, based on the analysis of field geolo-gical survey, geophysical prospecting, drilling, and large-scale direct shear tests, the authors consider that the formation mechanism of Chashushan landslide is complicated: rocks affected by the fault structure have the intensive development of rock mass structures and poor mechanical properties of rock and soil masses; the stratum system of landslide has a hydrogeologic structure of groundwater rich in the upper and poor in the lower, which is very vulnerable to landslide disasters. The stability of the landslide body is in critical condition due to heavy rainfall. Canal water infiltration influence of freezing-thawing action induced the occurrence of landslide. FLAC3D was used to simulate the stability of the landslide body. Results indicate that the landslide body has obvious signs of deformation under heavy rainfall and has formed intact slip surface, and the landslide is likely to occur again. Taking into account the formation mechanism of the landslide, it is effective for controlling the stability of the landslide body to strengthen the drainage and to avoid infiltration of the canal water.

    Petrology and Mineral Deposit
    The Magmatic Evolution and Its Constraints on Uranium Mineralization in the Xiaohuacha Uranium Deposit, Shaanxi Province
    LIU Gang, LIU Jiajun, YUAN Feng, ZHANG Shuai, SHA Yazhou, ZHANG Hongyuan, WANG Gongwen
    2017, 31(05):  990-1005. 
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    The Xiaohuacha uranium deposit is located in the northeastern section of the North Qinling Orogen. The uranium mineralization occurs within the assimilation and contamination area in the contact zone between the biotite granitic pegmatite and biotite plagioclase gneiss. To investigate the relationship between the granitic magma evolution and uranium mineralization, this paper presents detailed geochronological and geochemical studies of the granitoids. The results show that LA-ICP-MS zircon U-Pb ages of the Huichizi, Gaoshangou granites, and biotite pegmatites (uraniferous and non-mineralized zones) are (444±4.0) Ma, (422±0.82) Ma, (417±2.6) Ma, and (413±1.8) Ma, respectively. The granitoids are characterized by enrichment of large-ion lithophile elements (LILE), such as Rb, Ba, and K, but depletion of high field-strength elements (HFSE) such as Nb and Ta. High concentrations of Fe, Mg, and F in the uraniferous zone are interpreted to indicate chemical exchange between the pegmatitic magma and wall rocks in the assimilation-contamination area. The compositional heterogeneity in the individual biotite pegmatites is ascribed to the assimilation-fractional crystallization of pegmatitic magma. Interaction with the wall rocks in the contact zone triggers the destabilization of U-F complexes and precipitation of uraninite from the pegmatitic magma (ca.417 Ma) under favorable emplacement conditions. The assimilation of biotite plagioclase gneiss by pegmatitic magma during volatile saturation plays a main role in the formation of the Xiaohuacha uranium deposit.

    Genesis of the Wandao Gold Deposit in Guangxi, China: Evidences from Fluid Inclusions and H-O-S-Pb Isotopes
    LAI Xin, PANG Baocheng, LI Yuanqiang, ZHANG Qingwei, LÜ Jiawen, ZHOU Yequan, LI Peirong
    2017, 31(05):  1006-1021. 
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    The Wandao gold deposit, located in Gupao ore field of Dayaoshan polymetallic metallogenic clusters area in the southeastern Guangxi, is a medium-sized ore deposit discovered in recent years. The source of ore-forming substance and ore genesis are still under debate. There is still a big difference between its material origin and genesis. Based on detailed observation in underground tunnel and petrographic study under microscope, the Wandao gold deposit can be divided into W-Mo-Cu-Au mineralization period and main gold dominated mine-ralization period. Furthermore, the main gold dominated mineralization period can be divided into main stage and late stage. Microscopic temperature measurements and Laser Raman Spectra analysis of fluid inclusions in quartz indicate that the ore-forming fluids of main gold dominated mineralization period in the Wandao gold deposit are fluids with high temperature, low salinity, low density and containing CO2 and CH4. Hydrogen and oxy-gen isotope analysis data of quartz indicate the ore-forming fluids of main gold dominated mineralization period mainly derived from metamorphic water, and the ore-forming fluids of W-Mo-Cu-Au mineralization period is the mixture of magmatic water and metamorphic water. The small positive value of sulfur isotope for W-Mo-Cu-Au mineralization period infers that sulfur come from magma reservoir in depth. Whereas, small average with large range of sulfur isotopic composition for gold dominated mineralization period suggests that the sulfur in ore proba-bly mainly derived from strata and partly from magmatic rocks. Based on the above analysis, it is considered that the Wandao gold deposit belongs to metamorphic and magmatic hydrothermal superimposed deposit type.

    Paleontology and Stratigraphy
    The Rise of Atmosphere Oxygen and the Biological Evolution: An Important Geobiological Process
    MEI Mingxiang, MENG Qingfen
    2017, 31(05):  1022-1038. 
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    The rise of atmosphere oxygen that is chiefly resulted from the oxygenic photosynthesis illustrates a genetically consanguineous relation with the biological evolution. Microorganisms may also have played a major role in atmosphere evolution before the rise of oxygen, which shapes a microbial world before the Ediacaran. Even in today, these bacteria, as well as microscopic algae, supply oxygen to the atmosphere and churn out fixed nitrogen in Earth’s vast oceans. Earlier, less animal-influenced biospheres worked quite differently from the one currently occupied, with the Ediacaran-Cambrian radiation of organ-grade animals marking a fundamental shift in macroecological and macroevolutionary expression. Therefore, the rise of the atmosphere oxygen is actually a sophisticated geobiological process. Tracing the complex relationship between evolution and environmental change that is caused by the rise of the atmosphere oxygen will provide some important thinking approaches and researching clues for the further understanding of the sophisticatedly evolutionary history of the Earth.

    Geochemistry
    Thermodynamic and Kinetic Adsorption of Cr(Ⅵ) on Hydrochars and the Effect of Hydrothermal Time
    LIU Yuyan, ZHOU Jingyao, MA Shaoqiang, CHEN Jiawei
    2017, 31(05):  1039-1045. 
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    The agricultural wastes of peanut shells were used as carbonaceous material precursors, which were heated under the hydrothermal temperature of 200 ℃ and kept for the desired time duration of 1 h, 5 h or 10 h to prepare the hydrochars for the removal of Cr(Ⅵ) from aqueous solution. According to FT-IR spectrum, elemental analysis and SEM characterization of hydrochar samples, the results showed that hydrothermal carbonization method is feasible for porous carbon-based hydrochars, and the aromaticity increases with hydrothermal time, while the yield and the polar functional groups decrease.These properties would affect the adsorption performance of hydrochars. The batch experiments showed that the adsorption kinetics of Cr(Ⅵ) on hydrochars followed the pseudo-second-order model and the Freundlich model well fitted the isothermal adsorption. According to thermodynamic study, such sorption behavior belongs to a preferential easy process, which is also a spontaneous, endothermic and physical adsorption. The adsorption capacity of Cr(Ⅵ) on hydrochars were enhanced with the hydrothermal time on biomass of peanut shells. Therefore, hydrochars could be applied as an economic adsorbent in water remediation. The present study could also provide an important practical value for the comprehensive utilization of agricultural wastes.

    Oil-gas Exploration and Development
    Reservoir Characteristics and Distribution Rule of Weathering Volcanic Crust: A Case Study of the Carboniferous Volcanic Rock in Zhongguai Uplift, NW Junggar Basin
    FAN Cunhui, WU Qiang, DENG Yusen, LI Hu, HAN Yutian
    2017, 31(05):  1046-1058. 
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    Weathering volcanic crust reservoir has become an important and new field of oil and gas exploration, its characteristics and distribution rule are of great important theoretical and practical significance to the oil and gas exploration in volcanic rocks. Through comprehensive research of well drilling, cores, logs, seismic and laboratory analyses, weathering volcanic crust reservoir characteristics and distribution rule have been comprehensively studied from the volcanic rock formation environment in Zhongguai uplift, Junggar Basin. The result shows that volcanic rocks formed in the island-arc environment, and lithology is mainly andesite and tuff. The weathering crust structure of volcanic rocks can be divided into four layers: weathered clay layer, strong weathered zone, weak weathered zone and dense non weathered zone. The strongly weathered zone is the best of the four-layer structures, which is the main reservoir development zone. Reserving space mostly contains secondary pores and fractures, and the fracture has a better effect on reservoir seepage capacity. The development of reservoir is affected by lithology and lithofacies, tectonic movement, weathering and leaching, and fault(fracture). Carboniferous system volcanic oil-gas is mainly distributed along the three zones(close to fault zone, structural high part zone, beneficial lithofacies development zone), one side(near the plane of unconformity).

    Reservoir Characteristics of the Paleogene Mixed Carbonate-siliciclastic Rock or Succession and Its Influencing Factors in the Shizigou Area of the Western Qaidam Basin
    ZHANG Shiming, ZHANG Xiaojun, ZHANG Tingjing, WANG Pu, NAN Xixiang, GOU Yingchun
    2017, 31(05):  1059-1068. 
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    Western Qaidam Basin belongs to the sedimentary center of the saline lake basin in Qaidam Basin. Salinization stage of the western Qaidam Basin lasts for a long time, and the lake basin is widely distributed. Therefore the Oligocene lacustrine carbonate rock has great exploration potential. Based on core observation, rock slice identification, and the analysis of scanning electron microscope and electron spectrum of the samples of Shizigou area, the features of reservoir lithology,reservoir physical property and reservoir space are studied, and reservoir influential factors and forming mechanism are analyzed. The main conclusions are as follows. (1) The reservoir has characters of mixed deposit. The mineral composition is mainly carbonate and clastic grain, but neither of relative content is over 50%. The genetic type of mixed carbonate-siliciclastic rock or sucession is facies mixed. Fabric mixed is the main type, layer series mixed is the second type, and a few biological mixed type is found. The samples generally contain saline minerals. (2) The results of physical property analysis and X diffraction components testing show that the reservoir is super-low permeable and super-low porous, and its connectivity is poor. The content of carbonate rock composition is in the range of 10.9% to 47.0%, with an average of 32.1%. At the same time, porosity and carbonate content have a good positive correlation. (3) The reservoir space of the samples is mainly saline mineral dissolved pore, dolomite intercrystal pore and fracture. (4) The diagenesis of the reservoir is mainly cementation and dolomitization. Especially the cementation of the saline minerals suppresses the later diagenesis, forming local high pressure. The important conditions of dolomitization are high carbonate content and saline environments. The compaction of reservoir is weak. The reservoir experiences two cementation periods. The saline minerals which cementated in the later period are the main dissolution parts.

    Digital Core Modeling Construction of Different Lithofacies Shale: A Case Study of Dongying Depression
    CHEN Chen, LU Shuangfang, LI Junqian, ZHANG Pengfei, ZHANG Ping
    2017, 31(05):  1069-1078. 
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    Shale is a complex porous medium with low porosity, super-low permeability, tight and heterogeneity pore structure. The distribution of each component within shale can be visually revealed by the three-dimensional digital cores. Moreover, microscopic structural characterization and seepage simulation experiments of shale can also be carried out repeatedly and nondestructively using digital core. Therefore, the digital core is a more effective and convenient method than the conventional physics experiment methods for shale. The digital core constructed by the physical construction method is more accurate, however, which can only reveal the physical properties of a particular rock sample, and is generally effected by the contradiction between the field of view and resolution. Thus, it is necessary to construct the simple digital core models with a certain universality, which is constrained by some parameters, and can represent the characteristics of a kind of lithology or lithofacies. In the meantime, the current image segmentation methods are difficult to synthesize the multi-sample characteristics, which represent the characteristics of a kind of lithology or lithofacies. In this paper, we propose a method about threshold segmentation. It segmentalizes CT images based on the cumulative distribution function of image pixels, combined with the percentage of each component groups and the gray level distribution sequence. The volume relative content and gray level distribution sequence of mineral compositions and porosity of different lithofacies shale in Dongying depression are obtained by means of scanning electron microscopy (SEM) and energy-dispersive X-ray spectroscopy (EDX). And then the digital core models of different lithofacies shale, including rich felsic, felsic, rich calcareous, calcareous and rich argillaceous lithofacies shale, are constructed based on the X-ray computed tomography (CT) imaging. The results show that: (1) According to the grey value, the six component groups of shale reservoirs in Dongying depression from low to high,are followed by pore-fractures, organic matter, clay minerals, felsic minerals, calcium minerals and iron minerals, respectively;(2) Cumulative distribution function of pixels in CT gray image is represented cumulative distribution function of volume relative content of different lithofacies sample component groups. Based on volume relative content and gray level distribution sequence of different lithofacies shale sample components, threshold of each component group can be obtained in turn. This method is more suitable for threshold segmentation of specific lithofacies, while other segmentation methods cannot achieve; (3) The simple standard digital core models can be constructed by a superposition method. Firstly, the single-component digital cores are constructed based on CT images and thresholds of various petrographic component groups. And then these digital cores are superimposed together and the complete simple digital core is reconstructed, which is constrained by the parameters, such as mineral components and porosity. The simple standard digital core models, which have a certain universality, can represent the characteristics of a kind of lithology or lithofacies.

    Countermeasures Against Inter-bedded Barriers in SAGD Process
    SHI Lanxiang, LI Xiuluan, MA Desheng, LIU Pengcheng
    2017, 31(05):  1079-1087. 
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    Inter-bedded barriers sandwiched in heavy oil reservoirs have impacts on steam assisted gravity drainage (SAGD) performance. In the real SAGD operation, the impacts must be taken into full consideration and effective countermeasures against barriers must be studied to improve the SAGD oil production rate. In this paper, features of deformation of barrier rock under high temperature and high pressure conditions in the SAGD process were studied by coupled geomechanical numerical simulations with parameters gained from geomechanical tests of barrier rocks. The permeability of the barrier and the injection pressure of SAGD were determined to be main factors affecting the oil production rate of SAGD. Furthermore, two types of countermeasures against inter-bedded barriers, namely increasing injection pressure and vertical well assisted, were proposed, with characteristics of barriers and operational feasibility being taken into account together. And technical limitation and corresponding operation effect of each countermeasure were also provided. The results have an important guiding significance to the realization of economic and efficient development in SAGD process.

    Controls on High Water Production of CBM Wells in Shouyang Block, Qinshui Basin
    LÜ Yumin, LIU Yinghong, WANG Cunwu, GUO Guangshan, ZHU Xueshen, JIANG Rui
    2017, 31(05):  1088-1094. 
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    In order to reveal the controlling factors causing high water production of coalbed methane (CBM) wells in Shouyang block, Qinshui Basin, this paper makes a systematic analysis of the impacts of regional hydrogeological conditions, lithological association of coal seams and roofs and floors as well as aquifers, and fracturing techniques on water production of CBM wells, summarizes the geological risk and engineering risk leading to high water production, and finally brings in measures to avoid those risks. Results show that too high fracturing pumping rate is the immediate cause of high water production of CBM wells due to hydraulic connection between coal seams and aquifers, and high angle fractured aquifers nearby coal reservoirs in coal measure strata is the critical geological risk causing high water production of CBM wells. Additionally, unfavorable lithological association and regional hydrogeological conditions are the important factors causing high water production of CBM wells. Therefore, decreasing fracturing pumping rate, avoiding high angle fractured aquifers, and choosing coal seams which develops thick argillaceous roof and floors are the important measures to limit water production of CBM wells.