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    12 February 2021, Volume 35 Issue 01
    Typical Geohazards and Engineering Geological Problems Along the Ya’an-Linzhi Section of the Sichuan-Tibet Railway,China
    GUO Changbao, WU Rui’an, JIANG Liangwen, ZHONG Ning, WANG Yang, WANG Dong, ZHANG Yongshuang, YANG Zhihua, MENG Wen, LI Xue, LIU Gui
    2021, 35(01):  1-17.  DOI: 10.19657/j.geoscience.1000-8527.2021.023
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    The Sichuan-Tibet Railway is a major project being planned and constructed across the eastern part of Tibetan Plateau in China, where is characterized by extremely complex topography and geological structure. The active faults and frequent earthquakes are well distributed along the planned railway line, with ten large-scale regional active fault zones directly crossing or closely distributed along the newly planned Ya’an-Linzhi railway section, such as the Longmenshan fault zone, the Xianshuihe fault zone, and so on, of which the slipping rate could reach up to 10 mm/a, and with high potential risk of strong earthquakes. Under the coupling geological effect of internal and external dynamics, the geohazards are highly developed along the railway line, and densely developed along the Dadu River, Yalong River, Jinsha River, Lancang River, Nujiang River, Yarlung Zangbo River and their first-level tributaries, the active fault zones and the national highway. Especially, the long-runout landslides and geohazard chain, deep-buried creeping landslides, and earthquake-triggered landslides might cause more serious damages, which are the major challenges encountered in the railway construction. The railway is located in high stress environment dominated by horizontal tectonic stress, and there are about five major first-level stress zones along the railway and the adjacent area, i.e.,the south China main stress zone, the Longmenshan-Songpan stress zone, the Sichuan-Yunnan stress zone, the Motuo-Changdu stress zone and the Himalaya stress zone. The maximum principal stress direction of the Ya’an-Kangding railway section is the NWW-NW direction, and deflect into the NNE direction to Linzhi City. The regional stresses show strong differences in plane and vertical space, for example, there is a stress relief zone in the vertical direction of one tunnel revealed by in-situ stress testing results in Zheduo Mountain. Under the high geostress background, there are high risks of rockburst and large deformation in the deep-buried railway tunnels surrounding rocks. The railway construction should take safety distance from active faults, and strengthen necessary measures to monitor, early identify and predict the occurrence of giant geohazards, to measure and predict the geostress,large deformation and rockburst for deep-buried tunnel, which could provide scientific guidances for railway line selection and disaster prevention and mitigation.

    Analysis of Genetic Mechanism and Failure Mode of a Large Paleo-landslide in Sichuan-Tibet Railway Transportation Corridor
    WANG Jiazhu, GAO Yanchao, RAN Tao, TIE Yongbo, ZHANG Fan
    2021, 35(01):  18-25.  DOI: 10.19657/j.geoscience.1000-8527.2021.017
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    Sichuan-Tibet railway is vulnerable to serious geological hazards, especially where the topography is complex and tectonic activities are intense. The reactivation of paleo-landslides is one of the serious threats to the construction and operation of the railway. A paleo-landslide is located in the Kangding city, only one hundred meters away from the proposed Sichuan-Tibet railway. On the basis of the analysis of characteristics and formation mechanism using engineering geological mapping and exploration drilling, this study predicts its potential failure mode. The results are listed as follows. The large-scale paleo-landslide mainly slides along the bedrock-overburden discontinuity with strong partial deformation and develops multi-level tensile cracks. The stability scale is stable in the natural and rainy condition, but becomes unstable when earthquake occurs. The potential landslide failure sites are the trailing edges of gravel soil in the middle of the slope, while the potential sliding surface is the interface between the debris rock soil and the fully-weathered rock body.

    Landslide Susceptibility Assessment Based on Weight-of-Evidence Modeling of the Batang Fault Zone, Eastern Tibetan Plateau
    YAN Yiqiu, YANG Zhihua, ZHANG Xujiao, MENG Shaowei, GUO Changbao, WU Ruian, ZHANG Yiying
    2021, 35(01):  26-37.  DOI: 10.19657/j.geoscience.1000-8527.2020.091
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    The NE-SW-trending Batang fault is located in the eastern Tibetan Plateau, and has strong Holocene activity. Geological disasters such as collapses, landslides, and debris flows along the Batang fault zone are common. Through remote sensing interpretation and field survey, we established a landslide inventory over 10 km from both sides of the Batang fault, and a total of 93 landslide hazard points were identified. Based on the landslide geological background analysis, we summarized ten landslide susceptibility evaluation factors, i.e., topography (elevation, slope, aspect), topographic wetness index, lithology, meteorology and hydrology, active faults, engineering activities, and vegetation coverage. Weight-of-Evidence Modeling is used to calculate the landslide susceptibility. Using the receiver operating characteristic (ROC) curve accuracy of 82.3%, and the natural breaks-based method, the landslide susceptibility along the Batang active fault zone is divided into four levels(extremely high, high, medium, and low). The landslide susceptibility is mainly controlled by the Batang fault and river valley. The extremely high and high susceptibility zones are mainly distributed along the Batang fault zone and along the Jinshajiang and the Baquhe river valleys. The medium susceptibility zones are mainly distributed on both sides of the Baquhe tributaries. Low susceptibility zones are mainly distributed in high mountain areas with low engineering activities, and in relatively flat topography. The landslide susceptibility analysis results can well reflect the landslide development features along the Batang fault zone, and can provide scientific support for the major project construction and disaster prevention and mitigation.

    Numerical Simulation Study on Seismic Magnification Effect of V-shaped Deep-cut Valley on Sichuan-Tibet Railway Line
    QUAN Xuerui, HUANG Yehuan, LIU Chun, GUO Changbao
    2021, 35(01):  38-46.  DOI: 10.19657/j.geoscience.1000-8527.2021.020
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    V-shaped river valleys can produce ground motion amplification effects, and aggravate the destructive and disaster effects of earthquakes. Based on the high-performance discrete element software MatDEM, a numerical simulation study on the amplification effect of regular V-shaped valleys and real valley topography is carried out. The results show that for regular V-shaped valleys, when seismic waves are incident horizontally, the back-wave slope produces an obvious amplification effect of ground motion acceleration, and it is most intense near the valley bottom. The amplification effect increases as the valley slope angle increases. The numerical simulation results are consistent with analytical solutions in the trends and patterns, and agree with the field observation. The model is further applied in the analysis of the Rizha deep-cut valleys. It is found that small turning would affect wave propagation, and the acceleration amplification effect near the valley bottom is basically consistent with that of regular terrains. The discrete element method can effectively simulate the propagation, reflection, and scattering of seismic waves in river valleys. It can also be used for the analysis of dynamic and disaster effects under the complex conditions along the Sichuan-Tibet railway line.

    Development Characteristics and Formation Mechanism of the Xiongba Giant Ancient Landslide in the Jinshajiang Tectonic Zone
    LI Xue, GUO Changbao, YANG Zhihua, LIAO Wei, WU Ruian, JIN Jijun, HE Yuanxiao
    2021, 35(01):  47-55.  DOI: 10.19657/j.geoscience.1000-8527.2020.095
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    Xiongba giant ancient landslide is located on the right bank of Jinshajiang River (Gongjue County, Tibet), and located in the Jinshajiang active tectonic zone. The terrain and geological structure in this area is very complex, with many high mountains and gorges, large longitudinal slope drop, fragmentary rock mass, and a series of large and giant ancient landslides and slope deformation bodies were developed and pose serious hazards. On the basis of remote sensing interpretation and field investigation, we investigated the characteristics and formation mechanism of the Xiongba ancient landslide. We revealed that the accumulation volume of Xiongba ancient landslide is about 2.6×10 8-6.0×10 8 m 3, which is of giant scale in the regional geological history. The Xiongba ancient landslide comprises two large areas on the surface, i.e., the source area and accumulation area, among which the latter is divided into the relatively-stable zone and frontal-edge strongly-deformed zone. Through two deep-drilling on the landslide body, it is found that the Xiongba ancient landslide contains two-level deep creep slip zone:the shallow and deep slip zones have burial depths of 51 m (borehole ZK1) to 55 m (borehole ZK2) and 101 m (borehole ZK1) to 115 m (borehole ZK2), respectively. Hydrogeological conditions of the landslide body are complex with deep confined water developed, which greatly impact the slope stability. Our results show that the Xiongba ancient landslide may have formed under the coupling of internal and external dynamic factors, which include stratigraphic lithology, fracture activity, gravity, rainfall, groundwater, and river erosion. The landslide is currently creeping deeply, and the control of the “lock-up section” developed under the landslide platform is the key to the landslide stability. Under the influence of rainfall-groundwater seepage, river erosion and earthquake, the ancient landslide has a high possibility of instability, and may form a chain of disastrous events, such as blocking the Jinshajiang River and dam-broken floods.

    Stability Analysis and Prevention Countermeasures for Residual Bodies of Baige Landslide in Jinsha River
    ZHU Deming, LI Pengyue, HU Xiaohong, WU Xinming
    2021, 35(01):  56-63.  DOI: 10.19657/j.geoscience.1000-8527.2021.012
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    After the Baige landslide in Jinsha River experienced two times of sliding and blocking the river, the main body material of the landslide was greatly reduced, but there were still three large residual bodies in its trailing edge, i.e., K1, K2 and K3. Whether it has the possibility of again losing stability and blocking the river has become the focus of current work. The stability evaluation of landslide residues is mainly based on the factors of influence and the mechanism for the qualitative analysis, the results is more artificial due to the experience of the valuator. On the basis of field investigation, according to the engineering geological conditions and deformation characteristics of the area where the Baige landslide is located, seven factors such as slope height, slope angle, slope shape, free surface condition, groundwater seepage, fracture development and deformation were selected as evaluation factors, and based on AHP the fuzzy comprehensive evaluation model is used to evaluate the stability of the partition of Baige landslide. The evaluation results show that the stability of K1 and K2 residues is poor, and that of K3 residues is basically stable, which is in line with the actual survey status. The corresponding prevention and control countermeasures are put forward. The results can provide a valuable support for the evaluation and prevention of the same type of landslide.

    Early Landslide Detection in the Lancangjiang Region Along the Sichuan-Tibet Railway Based on SBAS-InSAR Technology
    ZHANG Jiajia, GAO Bo, LIU Jiankang, CHEN Long, HUANG Hai, LI Jie
    2021, 35(01):  64-73.  DOI: 10.19657/j.geoscience.1000-8527.2021.005
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    Early detection is a key to prevent and reduce geo-hazards. However, it is always problematic in complex topographic region, especially in alpine-valley region.Based on the Sentinel-1(ascending) and RADARSAT-2(descending) radar satellite data obtained from August 2018 to February 2020, quantitative detection and analysis of the potential surface deformation of landslides in the 80 km upstream and downstream of the Lancangjiang region along the Sichuan-Tibet railway was carried out by using the small baseline subsets in terferometric synthetic aperture radar(SBAS-InSAR). The results show that deformation rate in the LOS direction for the study period are from -58 to 21 mm/a (ascending) and from -42 to 16 mm/a (descending), respectively, and the maximum average deformation rate in the slope direction is -128 mm/a.Based on the deformation result in the slope direction, 113 potential landslides are detected,which are clustered in four regions. Besides, 13 landslides have significant deformation in the 113 potential landslides, deformation characteristics and slipping mechanism of the two critical landslide hazards were further analyzed. The results provide a reference for the route selection of Sichuan-Tibet railway,and for the geohazard prevention in the upstream/downstream of the Lancangjiang bridge. The technique of combining descending and ascending radar data can provide reference for early landslide detection in other alpine-valley regions along the Sichuan-Tibet railway.

    Characteristics and Potential Hazard of the Chada Collapse in Eastern Tibet
    LI Yuanling, LIU Jiankang, ZHANG Jiajia, GAO Bo, TIAN You, XIONG Deqing
    2021, 35(01):  74-82.  DOI: 10.19657/j.geoscience.1000-8527.2021.009
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    Featured by high speed, long transport and tremendous destruction, high-position collapses pose immense threats to the infrastructure, human lives and properties. The Chada high-position collapse was investigated in this study, and its development characteristics and potential hazards were analyzed through field investigation, remote sensing image analysis, unmanned aerial vehicle mapping and geophysical exploration. Our results show that the Chada high-position collapse involved a large rock volume 160×10 4 m 3 now located at the foot of the slope. The height difference of the collapse is 1,340 m. The maximum horizontal distance is over 2,600 m, and the maximum estimated speed is 65.36 m/s.This demonstrates that the collapse was of high-speed and long transport. The surface of the accumulation area is densely covered with boulders, and the accumulated rocks and soil display typical inverse grading feature. There are still 4.7×10 4-25×10 4 m 3 unstable rocks in the collapse source area. Induced by structural compression, freezing and thawing, long-term unloading and strong earthquake, the unstable rocks may fail and threaten the infrastructure and its ancillary facilities and villages. We suggested that geophysical exploration, costeaning and real-time monitoring should be conducted to assess the slope stability, initiating condition and probability of destabilization, and to predict and delineate the affected region. According to the evaluation results, appropriate measures should be conducted for hazard prevention.

    Development Characteristics of Chada Debris Flow in Southeast Tibet and Its Influence on the Proposed Station
    HUO Xin
    2021, 35(01):  83-91.  DOI: 10.19657/j.geoscience.1000-8527.2020.108
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    In view of the influence of debris flow disaster on the site selection of Sichuan-Tibet railway station, based on field investigation and remote sensing interpretation, on the basis of ascertaining the current situation of debris flow, this paper analyzes the formation mechanism of debris flow from the material source, induced factors, dynamic factors and other disaster conditions, and calculates the dynamic parameters of debris flow. The velocity of Chada debris flow at the mouth of the gully is 7.63 m/s, the static and dynamic reserves are respectively 15.198,1 million m 3 and 38.08 million m 3 and the risk degree of debris flow is 0.5. It is determined that the debris flow is large-scale-viscous-rainstorm-gully-developing-medium-prone-moderate dangerous debris flow. In view of the fact that the mud-rock flow of Chada directly affects the site selection of Luolong station of Sichuan-Tibet railway, considering two different engineering settings of bridge and tunnel, in order to determine the appropriate route scheme, four schemes are selected. The comparison results show that there is no silting risk in the deck of DK scheme of bridge engineering, the risk of partially or completely blocking the bridge culvert aperture is low, and it is convenient to build protective works such as drainage channel, etc. the risk caused by debris flow is controllable, which is the optimal scheme. The research results of this paper can provide reference for the selection of railway station sites under similar conditions in this region.

    Optimization of Disaster-reduction Route Selection in Geological Disaster-Prone Region Along the Sichuan-Tibet Railway Based on Virtual Reality: A Case Study of Luolong Station
    ZHOU Jie, DING Mingtao, HUANG Tao, CHEN Ningsheng
    2021, 35(01):  92-102.  DOI: 10.19657/j.geoscience.1000-8527.2021.014
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    The frequent landslide and debris flow disasters along railway lines have obvious negative impacts on the railway construction and safe operation, and hinder social and economic development. During the railway route design process in mountainous regions, how to scientifically plan the line location and project scheme, and to assess the railway geological risk, has become a common concern to researchers around the world. Therefore, this paper introduces a visual simulation for railway disaster-reduction route selection scenarios in geological disaster-prone areas, on the basis of virtual reality (VR). The system first uses CAD, Sketch Up and other software to establish three-dimensional (3D) terrain environment model. According to the simulation results on landslide and debris flow disaster evolution along the railway line, the virtual railway model of the study area is built based on the Unity3D platform using 3Ds Max, Photoshop, and other software. Finally, the 3D visualization of virtual railway and terrain roaming is performed through the interactive Web interface design. Taking the Luolong station of Sichuan-Tibet Railway as an example, a variety of route schemes are established with this method. The results show that the established VR scenario has good visibility and smooth interactivity, which can fully assess the feasibility of construction and operation safety of the local mountain railway.

    Development Characteristics and Deformation Monitoring Analysis of the Zhouchangping Landslide in Maoxian County, Sichuan Province
    JIN Jijun, GUO Changbao, SHEN Yaqi, YANG Zhihua, REN Sanshao, LI Xue
    2021, 35(01):  103-113.  DOI: 10.19657/j.geoscience.1000-8527.2020.102
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    The Zhouchangping landslide in Nanxin Town (Mao County, Sichuan Province) is a large-scale ancient landslide, which had an extensive and rapid reactivation in 1982. At present, the sliding body appears as irregular tongue-shaped on the surface, with a length of about 850 m and height difference of about 350 m between its frontal and rear edge. Three levels of sliding were developed on the profile. Drilling revealed that the burial depth of slip zone is mainly 50-70 m, and the volume of potential unstable landslide is estimated to be about 1,500×10 4-2,000×10 4 m 3. The Zhouchangping landslide is divided into four deformation zones. A large number of tensile cracks and downward dislocation scarps are developed at the toe of the middle-rear part and front-edge of the sliding body. The tensile cracks are mainly 0.2-3.0 m wide, and the downward dislocation of the scarps is 2-10 m. Based on field investigation and drilling, we monitored the surface displacement (GNSS), deep-creep deformation (borehole inclinometer) and rainfall on the landslide. Our data (collected across one year) demonstrate that the current deformation rate of the rear edge of the landslide is 0.80 m/a, and those of the middle and frontal edges are 0.69 m/a and 0.51 m/a, respectively, showing a push-type sliding deformation toward 310°. The surface displacement rate fluctuates from 1 to 3 mm/d during the monitoring period, and the fluctuation was mainly influenced/delayed by rainfall. The slip acceleration fluctuates from 0 to 6 mm/d 2. Data from ZK2 borehole inclinometer shows that the landslide mainly crept along two layers of slip zones in the 80 m depth, of which the burial depth of shallow and deep slip zone is about 22 m and about 46 m, respectively, with the slip rate fluctuating between 0 and 5 mm/d. Comprehensive study shows that Zhouchangping landslide is currently in the deep-creep stage with slowing deformation. Its deformation rate is affected by factors such as rainfall and river erosion. Under extreme internal and external dynamic conditions, the slope sliding may accelerate and reactivate again, causing incidents such as blocking of the Minjiang River.

    In-situ Stress Measurement and Its Application of a Deep-buried Tunnel in Zheduo Mountain, West Sichuan
    XU Zhengxuan, MENG Wen, GUO Changbao, ZHANG Peng, ZHANG Guangze, SUN Mingqian, CHEN Qunce, CHEN Yu
    2021, 35(01):  114-125.  DOI: 10.19657/j.geoscience.1000-8527.2021.018
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    Characteristics of present stress state at a deep-buried tunnel in Zheduo Mountain (west Sichuan) are analyzed based on in-situ stress measurement results at 196-650 m depths using the hydraulic fracturing me-thod. The measured results show that the stress state is dominated by horizontal principal stress, which increases linearly with depth and with higher gradient than the Chinese mainland background value. Reverse stress regime (SH>Sh>Sv) is dominant overall within the measurement depth. The stress-release zone is at 389.50-560.50 m depth, and the stress regime is mainly strike-slip with relative principal stress magnitude of SH>Sv>Sh. The lateral pressure coefficients and the ratio of maximum and minimum horizontal principal stress corresponds approximately with the variation characteristics of Chinese mainland. The fracture impression results reveal that the maximum horizontal principal stress is predominantly WNW, consistent with the regional stress field and mechanical mechanism reflected by the surrounding active faults. Stress field in the study area is mainly controlled by the ongoing India-Asia continent-continent collision and the compressive tectonics from the growing Tibetan Plateau onto the rigid Sichuan Basin. The test borehole is nearly critically stressed in the current stress state. The optimal-orientated plane or special section of the exiting faults may experience instability sliding with the continuous stress accumulation. Subsequently, tunnel stability from the in-situ stress perspective is discussed. The results reveal that the deep-buried tunnel favors medium-strong rock-burst due to strong in-situ stress state and deep burial, and the optimized design and constructive protection should be focused.

    In-situ Stress Measurement of Guodashan Tunnel Horizontal Borehole in West Sichuan and the Engineering Significance
    SUN Weifeng, GUO Changbao, ZHANG Guangze, ZHANG Yongshuang, XU Zhengxuan, TAN Chengxuan, LI Dan, WANG Xianli
    2021, 35(01):  126-136.  DOI: 10.19657/j.geoscience.1000-8527.2021.021
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    The newly built Sichuan-Tibet railway line extends across the Xianshuihe active tectonic zone, along which the tectonic stress field is extremely complex, and the risk of tunnel rock engineering failure is prominent. To reveal the local tectonic stress-field, to provide basic parameters for deep-buried tunnel design and construction, and by using the recently-developed hydraulic fracturing in-situ stress measurement instrument, a total of 10 valid in-situ stress data were obtained from the Guodashan tunnel horizontal borehole (maximum borehole depth: 508.10 m), creating a new record of hydraulic fracturing in-situ stress measurement in horizontal borehole. Our results show that at the borehole depth of 148.4 to 508.10 m, the maximum principal stress is 3.59-13.72 MPa, whilst the minimum principal stress is 3.28-8.36 MPa along the borehole section plane.According to the fracture impression results, the dip of the maximum principal stress along the borehole section plane is approximately horizontal in the deep part of the borehole, except for the shallow part of the borehole where the maximum principal stress is steep.According to the in-situ stress state of the horizontal borehole, we located the stress-releasing zone at 0 to 280 m depth, the stress-concentration zone at 280 to 330 m, and the undisturbed-stress zone at above 330 m depth. Based on the in-situ stress measurement results, wallrock stability of the Guodashan tunnel was analyzed. The analysis reveals that the wallrocks would experience slight to moderate rockburst at only 292.9 m and 508.10 m depth.

    Failure Modes and Influence of Interlaminar Fracture Zone Connectivity on Slope Stability of Bedding Rock Slope in Ya’an, West Sichuan
    ZHOU Hongfu, RAN Tao, CHEN Bo, GAO Shu, WU Wenxian
    2021, 35(01):  137-144.  DOI: 10.19657/j.geoscience.1000-8527.2021.011
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    Bedding rock slope is a common slope type in sedimentary rock areas, and is a slope-type that is focused on by various engineering construction. Taking a typical bedding rock slope in Ya’an area of west Sichuan as an example, the deformation and failure modes of the slope are summarized by field investigation, UAV mapping, drilling, geophysical exploration, stability calculation and other technical methods. The relation between the connectivity of interlaminar fracture zone and slope stability under different conditions is analyzed and calculated. The results show that: the interlaminar fracture zone has an important influence/control on slope stability. When the connectivity of the interlaminar fracture zone in the shallow part of the slope is less than 86%, the slope stability is consistent with the current investigation results. This provides a new idea to analyze the extension length or connectivity of interlaminar fracture zone of layered rock bodies. The research results have important engineering significance for infrastructure planning and construction, as well as for disaster prevention and mitigation in west Sichuan.

    Geological Structure and Rock Deformation Characteristics and Their Geohazard-Controlling Mechanism in Yajiang Area, West Sichuan
    XIONG Xiaohui, BAI Yongjian, TIE Yongbo
    2021, 35(01):  145-152.  DOI: 10.19657/j.geoscience.1000-8527.2021.007
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    Structural patterns of compound anticlines and synclines with faults superimposed are widely developed in Yajiang area, west Sichuan. Due to intensive tectonic reworking, at least seven rock deformation types present in the study area, including flexible slippage, bedding shear, brittle bending, unloading along structural planes, large-scale dislocation, fault fracture and fold cleavage. Structural-lithologic assemblage has shaped the distribution of Yalong river and valley evolution. Meanwhile, the development and distribution of geohazards, e.g., landslides and collapses, and their stability and risk are controlled by valley evolution and tectonic reworking. The different of geohazard types are controlled by various rock deformation types, and the lithologic association has constrained their size. Interbedded sand-slate controlled by brittle bending has often experienced toppling-drawing breakage-slippage-unstable failure-river blockage, and the multistage slope evolution represents the main geohazard model in Yajiang area.

    Creep Characteristics and Constitutive Model of Gneiss in Zilashan Area Along Sichuan-Tibet Railway Line
    WANG Lei, GUO Changbao, GUO Pengyu, JI Feng
    2021, 35(01):  153-160.  DOI: 10.19657/j.geoscience.1000-8527.2021.008
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    Gneiss is widely distributed in the Zilashan area along Sichuan-Tibet railway line, and the anisotropic characteristics of the rocks are remarkable. During the construction of deep-buried tunnels, wallrock deformation directly affects the stability and reinforcement measures. To reveal the creep characteristics of gneiss from the Zilashan area in western Sichuan to eastern Tibet, triaxial compression creeping tests were carried out. Therefore, an abnormal crack propagation phenomenon was discovered. Based on the superposition principle, the long-term strength was determined by drawing an isochronous stress-strain curve. Using the Burgers model, a creep constitutive model that is more suitable for engineering practice was established. The parameters were then identified through L-M algorithm and global optimization. The results clearly show that under the same confining pressure condition, instantaneous strain increment of the samples decreases with increasing stress level, and consequently hardening occurred. From the sample creep characteristics, the phenomenon of abnormal crack propagation caused by microstructure anisotropy occurs, and the sample creep rate increases sharply due to abnormal crack propagation in the attenuation creep stage. The long-term strength increases with peristaltic pressure. Compared with the conventional triaxial test, the long-term strength decreases by 59.8% and 21.3%, respectively, and the improved Burgers model is more practical. The mechanical testing parameters can form a scientific basis for engineering construction and disaster prevention and control.

    Experimental Study on Influence of Confining Pressure and Water Content on Dynamic Strength of Slate Residual Soil
    WANG Lei, GUO Changbao, LI Bin, HUANG Xin, ZHENG Zhihua, WANG Jiaqi
    2021, 35(01):  161-166.  DOI: 10.19657/j.geoscience.1000-8527.2021.019
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    Under the influence of special geotectonic conditions, the slate and phyllite in western Sichuan-eastern Tibet are strongly weathered, and the residual soil is widely distributed. It is of great practical significance to study the dynamic characteristics of metamorphic rock-derived, highly-weathered soil in this area. In this study, dynamic triaxial experiment was carried out on the slate residual soil from the region. The results show that the moisture content and confining pressure have obvious influence on dynamic strength of the samples. Under the same consolidation stress and consolidation ratio, the strength decreases with increasing water content. Under the same moisture content and consolidation ratio, the strength increases with increasing consolidation stress, but the correlation is not proportional. The dynamic cohesion of slate residual soil decreases with increasing water content, and the former is highly sensitive to the latter. However, the dynamic friction angle has little changes with increasing water content and is less sensitive to the latter.

    Tectonic Stress Field and Engineering Influence of China-Nepal Railway Corridor
    MENG Wen, GUO Changbao, MAO Bangyan, LU Haifeng, CHEN Qunce, XU Xueyuan
    2021, 35(01):  167-179.  DOI: 10.19657/j.geoscience.1000-8527.2020.104
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    The proposed China-Nepal railway is located in the India-Asia collisional-compressive front, which is characterized by regional active faulting, frequent earthquakes, strong neotectonic activities, and complex stress fields.Characteristics of the present-day stress field in the railway corridor and its effects on tunnel stabi-lities is analyzed based on the focal mechanism solutions and in-situ stress measurements. The results show that the local principal compressive stress at the seismogenic depths is ENE along the plate boundary, compared with the heterogeneous stress field inside the Plateau. The Chinese (Xigaze to Jilong) section is mainly in tensile-shear stress field, while the Nepali section is in compressive stress field controlled by the India-Asia collision. Given that there is no in-situ measurement in the China-Nepal railway corridor, we analyzed the shallow stress field based on the measured data in the neighboring areas. Stress regime in the shallow crust is generally conducive to reverse faulting, and the maximum horizontal principal stress is predominantly NE. Based on the distribution characteristics of principal stress direction, the China-Nepal Railway comprises six sections, and the possibility of the wallrock burst is discussed,considering both stress field analysis and σθmax/Rc theory.We concluded that a larger angle between the maximum horizontal principal stress direction and the axial direction of the tunnel is detrimental to the wall rock stability:The greater the tunnel depth, the greater the rock burst possibility.Most sections of the China-Nepal railway intersect the maximum horizontal principal stress axis at a large angle or even nearly perpendicular. Rock bursts likely occur when the tunnel is deep, and major protection measures are required.This study provides scientific reference for railway engineering survey and routeselection.

    Preliminary Prediction of Temperature Field and Thermal Damage in Zheduoshan Region Along Sichuan-Tibet Railway
    ZHAO Zhihong, XU Haoran, LIU Feng, WEI Shuaichao, ZHANG Wei, WANG Guiling
    2021, 35(01):  180-187.  DOI: 10.19657/j.geoscience.1000-8527.2021.022
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    Heat harm is a common geological hazard in Sichuan-Tibet railway, China. Zheduoshan region is located in the Kangding geothermal field with abundant geothermal resources, which may induce severe thermal damages. Due to the poor traffic and construction conditions in plateau mountainous area, drilling and other geophysical surveys cannot be easily applied. To precisely predict the surrounding rock temperature along the tunnel and compensate for the lack of geological exploration in difficult terranes, a numerical model of tunnel A along the railway line is built and calibrated based on geological data. Faults, lithology, geothermal temperature, groundwater, and other factors are considered in the model based on geothermal theory. The temperature distribution in the surrounding rocks of the tunnel is revealed. In addition, we evaluate the thermal damage risks along the planned tunnel, which would be useful for its site selection, design and construction.

    Geochemical Characteristics of Medium-high Temperature Geothermal Fluids in West Sichuan and Their Geological Implications
    ZHANG Wei, WANG Guiling, ZHAO Jiayi, LIU Feng
    2021, 35(01):  188-198.  DOI: 10.19657/j.geoscience.1000-8527.2021.015
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    West Sichuan is one of the main high-temperature geothermal resources distribution areas in China. The space-time distribution and material source of hydrothermal activities are closely related to hydrothermal diagenesis. The geochemical characteristics of geothermal fluid reflect the deep geochemical process information during the process of fluid rising to the surface. The fluid chemical characteristics of typical geothermal fields at Xianshuihe, Ganzi-Litang, and Jinshajiang along the fault zone are compared and analyzed. The results show that the groundwater type in the area is HCO3-Na. K +, Na +, HCO3 - and Mg 2+ in the geothermal water of Ganzi-Litang have similar material sources as Cl -, and they come from the deep earth besides mineral dissolution. The geothermal fluid runoff in the study area is long, with the depth of 2,189.93-5,620.52 m. The proportion of cold water mixed into geothermal fluid is 56%-78%, thus, the water rock interaction has not yet reached the equilibrium state. During the circulation process, it is affected by the dissolution of silicate minerals containing calcium and magnesium. The fluid path convergence and controlling factors are clarified. The results enhance the understanding of geothermal resource distribution patterns and genesis in west Sichuan, and provides reference for engineering construction in the region.

    Formation Model of Geothermal Water in Chaya of Tibet: Perspective from Hydrochemistry and Stable Isotopes
    ZHANG Chunchao, LI Xiangquan, MA Jianfei, FU Changchang, BAI Zhanxue
    2021, 35(01):  199-208.  DOI: 10.19657/j.geoscience.1000-8527.2021.013
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    Two occurrences of geothermal waters have been identified in Chaya of Tibet, and the one at Niangqu has a flow rate of 23,356 m 3/d and a temperature of 36 ℃. Understanding its hydrochemical and isotopic characteristics and groundwater circulation model is of great significance to tunnel design and construction. To clarify its hydrochemical characteristics and formation model, we analyzed the isotope hydrochemistry of water samples from these two geothermal water occurrences. The two geothermal waters contain main cations of Ca 2+ and Mg 2+, main anions of SO42- and HCO3-. They are classified into SO4-Ca·Mg and SO4·HCO3-Ca·Mg water-type, and have TDS content of 1,255 to 2,051 mg/L. Stable hydrogen and oxygen isotopes indicate that the main source of geothermal waters is meteoric precipitation, as featured by a 18O drift, reflecting O-isotope exchange between hot water and the wall rocks. Elevation of the recharge area is of 4,146 to 4,185 m, the temperature of the geothermal reservoir is about 53.1 to 61.0 ℃, and the water circulation depth is approximately 1,409 to 2,020 m. Formation model of the geothermal water is proposed as follows: after receiving recharge from meteoric water infiltration in high mountainous area from the northeast, groundwater may have flowed along the fractures between the karst layers and was heated by the geothermal heat flow through deep circulation. The water may have risen along faults due to the aquitard structure, mixed with 0.79 to 0.91 shallow groundwater, and formed springs in valley topographic incision. Integrating hydrogeology and tunnel location, the eastern karst-rich water area poses less threat on tunnel water incursion. The western karst-rich water area has tectonic karst water for the tunnel, and the risk of high-pressure water incursion should benoticed.

    Analysis of Geothermal Origin in Eastern Himalayan Syntaxis
    MA Xin, FU Lei, LI Tiefeng, YAN Jing, LIU Ting, WANG Mingguo, SHAO Wei
    2021, 35(01):  209-219.  DOI: 10.19657/j.geoscience.1000-8527.2021.016
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    The eastern Himalayan syntaxis is one of the regions with the strongest tectonic activity and the fastest geomorphic evolution on the Earth. It belongs to the Mediterranean-Himalayan tropics with strong hydrothermal activities. Based on the geological background, the development characteristics and genetic model of the deep underground hot water at Jiali are preliminarily explored through field survey, hydrochemical and stable isotope analyses. The results show that the origin of local geothermal water comes from meteoric precipitation or ice/snow melting, and the recharge altitude is above 4,500 m. It is speculated that the recharge area is located in the mountainous gneissic region in the northwest of the study area. The geothermal water in the area is immature. The geothermal water replenishment source circulates along the faults to the deep thermal reservoir, and then ascends by heating and convection until it is exposed as hot springs. The geothermal water rises to the shallow surface and mixes with cold water at a mixing ratio reaching 91%. SiO2 thermometer, cation thermometer and silicon-enthalpy models are used to estimate the reservoir temperature, and the maximum reservoir temperature is 380 ℃. The depth of geothermal water circulation reaches 6,900 m in the Yarlung-Zangbo River junction zone. The local geothermal heat source comes mainly from the Yarlung-Zangbo River junction zone and the nearby deep faults, and the surface geothermal springs are mainly controlled by the secondary tensile and torsional faults on both sides of the junction zone. This study preliminarily revealed the geothermal genetic model at Jiali of the eastern Himalayan syntaxis, which can provide a scientific basis for the geothermal resource development and utilization, and for the planning and construction of major projects in the area.

    Multi-stage Characteristics and Tectonic Significance of the Jiali Fault in Guxiang-Tongmai Section, South Tibet
    ZHAO Yuanfang, GONG Wangbin, JIANG Wan, CHEN Longyao, QIU Duwei
    2021, 35(01):  220-233.  DOI: 10.19657/j.geoscience.1000-8527.2021.010
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    The Jiali fault is an important part of the WNW-ESE trending Karakorum-Jiali fault system in the southern Tibetan Plateau, which is considered to be an ancient suture zone between the north Lhasa and the central Lhasa block. However, the tectonic properties and deformation ages of the Jiali fault are still controversial and need further study. Based on detailed regional geological mapping, our work focused on the Guxiang-Tongmai section of the Jiali fault, especially on investigating the geometric and kinematic characteristics, and subsequently on restoring and calculating the stress field and their direction in different periods, based on the newly identified fault planes and striations of different directions. Accordingly, we analyze the superimposing structural relations of this area, and discuss the multi-stage activity characteristics of the Jiali fault under different tectonic stress fields, and the regional tectonic evolution and background. Consequently, the influence of the Jiali fault on the proposed Sichuan-Tibet railway line was discussed. Results indicate that the Jiali fault is active from the Late Cenozoic, and show tectonic superimposed characteristics, including (from early to late) the sinistral strike-slip fault (D1), normal fault (D2) and dextral strike-slip fault (D3). As an important accommodation structure of the eastern Himalayan syntaxis, the multi-stage deformation of the Jiali fault zone reflects the relative movement of adjacent blocks and the regional tectonic stress field conversion, which is of great significance for understanding the Cenozoic tectonic evolution of the southern margin of Tibetan Plateau.

    Evaluation on the Importance of Ecological Protection in Changdu Section of the Sichuan-Tibet Railway
    WANG Siyuan, ZHAO Minmin, YAN Jing, MA Xin, DIAO Yujie, FU Lei, LUO Qian
    2021, 35(01):  234-243.  DOI: 10.19657/j.geoscience.1000-8527.2021.006
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    The Sichuan-Tibet railway extends across many geographical units, which is of great ecological protection significance. Effective protection of the ecological environment along the railway is a key issue during the process of railway planning, construction, and operation. In this study, the Changdu section of the Sichuan-Tibet railway is studied. The ecosystem service function and sensitivity are important in measuring the quality of ecosystem and establishing high-quality ecological conservation protocols. This study integrated data analysis and field investigation, and evaluated the ecosystem service and ecological vulnerability of the research area through ecological evaluation modelling, and evaluated the importance of the ecological protection along the railway line based on the research results. The results show that the percentage of the most important, important, and generally important ecological protection areas along the Changdu section is 42.19%, 52.69% and 5.12%, respectively. The evaluation results can assist engineering activity planning during the railway design, construction, and operation, and reduce the negative impact on the ecosystem in a targeted way, and achieve a win-win scenario for the social, economic, and ecological benefits.

    Ore Deposits and Geochemistry
    Fluid Evolution and Mineralization Mechanism of Dongchuan Copper Deposit in Yunnan Province
    ZENG Ruiyin, JIANG Hua, ZHU Xinyou, ZHANG Xiong, XIAO Jian, LÜ Xiaoqiang, HU Chuan, YANG Xiaokun, LI Jinlin, ZHEN Zheguang
    2021, 35(01):  244-257.  DOI: 10.19657/j.geoscience.1000-8527.2021.01.25
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    Dongchuan copper deposit is important sediment-hosted stratiform copper deposits (SSC) in China, which has remarkable multilayered metallogenic characteristics and typical copper sulfide zoning. In this study, the fluid inclusions of copper ore from different layers were analyzed by microthermometry and laser Raman spectrum. The results show that: two types of inclusions are distinguished in the copper ores of Dongchuan Group, which are the light-colored and the dark-colored inclusions. The composition of light-colored inclusions is dominated by H2O, riching in halite, a small amount of sylvite, and anhydrite crystals, which represents oxidized ore-bearing brine, coming from dissolution of marine evaporate and formation water between strata.Microthermometry analysis shows that the ore-forming brine has the characteristics of low-medium temperature (140-300 ℃), middle-high salinity (12%-44%), and belongs to Na +-K +-Ca 2--Cl -(SO4 2-) basin brine. The dark-colored organic inclusion represents reduced fluid, which comes from the carbonaceous slate of Heishan Formation and the algal organism decomposed Luoxue Formation. Dongchuan copper deposit took the stromatolite-rich sandstone dolomite of Luoxue Formation as the precipitation system, and the carbonaceous slate of Heishan Formation as the barrier layer, forming a fluid closed physicochemical trap. The oxidized ore-bearing brine was transported to the reductive precipitation system through the supply system, and mixed with the reduced fluid and the organic-bearing stratum, and formed the sediment-hosted stratiform and veined copper orebodies.

    Geochemical Characteristics of Primary Halos and Deep Prospecting Prediction of the Shijia Gold Deposit in Penglai, Shandong Province
    ZHANG Yingshuai, GU Xuexiang, ZHANG Yongmei, WANG Jialin, FENG Liqiang, GE Zhanlin, HE Yu
    2021, 35(01):  258-269.  DOI: 10.19657/j.geoscience.1000-8527.2021.01.26
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    In order to predict and evaluate the deep prospecting potential of the Shijia gold deposit in Penglai of Shandong Province and to prolong the service life of the mine, this paper aims to describe the geochemical cha-racteristics of primary halos in the deposit and to discuss the deep prospecting potential of the deposit. Analysis of the characteristics of element association indicates that the combined elements of the orebodies and near-ore halos include Au, Ag, Cu, Pb, Zn, S, and Te, those of the front halos are Hg, As, Sb, Ba, and those of the tail halos consist of Mo, W, and Sn. The characteristics of element anomalies for the ore vein 326 show that the front and near-ore halos are dominant in the south, and the front and tail halos are dominant in the north while the near-ore halos is weak. The orebody is overall characterized by plunging southward at depth. The reverse zoning and coexistence of front halos and tail halos appear in the axial zoning sequence of primary halos along the prospecting lines 36 and 84. Combined with the characteristics of vertical oscillation and fluctuation of geochemical parameters, it is suggested that the ore bodies formed during multiple mineralization stages and may extend to the depth with blind ore bodies. Comprehensive analyses show that the southern section of the ore vein 326 is favorable for mineralization with a good potential for prospecting space in its deep sites. Although the deep mineralization in the northern section is weakened, the coexistence of front and tail halo elements indicates that there still may exist blind orebodies in its deep space.

    Anomaly Characteristics of 1:50,000 Stream Sediments Survey and Analysis on Prospecting Effect in Mengweng Area, Yunnan
    ZENG Kai, LIU Hai, HUANG Dejiang, GUO Wei, QI Shuanglin, SI Xiaohua, YANG Yuzhen
    2021, 35(01):  270-280.  DOI: 10.19657/j.geoscience.1000-8527.2021.01.27
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    Mengweng area of Yunnan Province is located at the southern end of Lincang-Menghai rare earth-polymetallic mineralization subzone, where granite weathering crust is well developed and rare earth mineralization conditions are favorable.In order to coordinate the geological survey of the mineral resources in the area and narrow the scope of prospecting, 1:50,000 stream sediment survey for rare earth minerals was carried out in the area, this paper summarizes the geochemistry distribution, enrichment, element combination and anomaly of 29 elements, including La, Y and Zr, and delineates the comprehensive anomaly.The analysis shows that La, Y, Zr, W, Sn and Au are the main ore-forming elements in the area.The anomaly of La, Y and other related elements such as F, P are well nested, and its abnormal characteristics are obvious.On the basis of the mea-surement of stream sediments, the work of anomaly verification and mineral inspection was carried out, and delineation of three prospecting targets, one of them was transformed into a newly discovered ore producing area, and good prospecting results have been obtained.

    Application of High-resolution Chemical Sequence Stratigraphy to Deep-water Fine-grained Sediments:A Case Study of Wufeng Formation and Lower Member of Longmaxi Formation in Liutang Outcrop, Upper Yangtze Area
    WANG Qian, HUANG Yongjian, ZHANG Zhifeng, WANG Changhong, LI Xiang, LIU Wei
    2021, 35(01):  281-292.  DOI: 10.19657/j.geoscience.1000-8527.2021.01.28
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    Based on the theories and methods of chemical stratigraphy and sequence stratigraphy, the data of Liutang outcrop profile and sample analysis and test in Shizhu County of Chongqing are used to optimize the indicators system for the chemical sequence stratigraphic division which are the elements assemblages of Al-K-Ti-Rb-Cr-Zr, related to input intensity of terrigenous, the elements assemblages of Ca-Mn-Mg-Ba-Zn, related to autogenetic precipitation intensity, and the elements assemblages of V-Ni-Mo-U-As related to organic matter adsorption and deoxidation intensity. The Wufeng Formation of Liutang outcrop is divided into LCW sequence, and the lower part of Longmaxi Formation is divided into MCL1-1, MCL1-2, MCL1-3, MCL1-4 sequences upwardly. The total amount of major and trace element combinations related to the input intensity of terrigenous source is relatively high near the sequence boundary, but relatively low near the most oceanic flooding surface, which has the cyclic changes characteristics of decreasing-increasing of total elements. However, the total amount of major and trace element assemblages related to autogenetic precipitation, organic matter adsorption and deoxidation intensity are generally lower near the sequence boundary and higher near the maximum flooding surface, which has the cyclic changes characteristics of increasing-decreasing the total amount of elements. The cyclic change characteristics of the total amount of element assemblages with different genetic signi-ficance is the response of regional sea level change, which has regional consistency and can be used as the basis of regional stratigraphic correlation.

    Distribution Characteristics and Influencing Factors of Soil Cu in Jieyang City, Guangdong Province
    HUANG Changchen, WEN Hanhui, CAI Limei, LUO Jie, JIANG Huihao
    2021, 35(01):  293-300.  DOI: 10.19657/j.geoscience.1000-8527.2021.01.29
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    Taking soil collected from Jieyang, Guangdong, China as the study object, the Cu content of 1,330 surface soil samples (0-20 cm) and 331 deep soil samples (150-200 cm) were measured, and the distribution characteristics and influencing factors of soil Cu were studied accordingly. The enrichment factor, GIS spatial analysis and variance analysis were used to comprehensively analyse the enrichment characteristics, spatial distribution characteristics and influencing factors of soil Cu in the study area, and the risk of soil Cu pollution was evaluated according to national standards. The results showed that the average Cu content of surface soil was 9.49 mg/kg, which was far lower than the Cu risk screening value (50 mg/kg) in the “Soil Environmental Quality Risk Control Standard for Farmland Soils (Trial) (GB15618-2018)”. The enrichment degree of copper in surface soil was at the level of non-enrichment and slight enrichment, and there was no obvious copper enrichment. The high value areas of copper in surface soil were mainly distributed in the central Rongcheng district, southeast Jiexi County, and west and north Huilai County. Soil parent material and land use pattern were the main influencing factors of copper content in the surface soil of the study area, and soil type also had certain influence on it. In different parent materials, the Cu content in the Quaternary sediments was the highest; Under different land use types, the Cu content of construction land was significantly higher than other land use types; In different soil types, the Cu content in paddy soil was the highest.