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    20 October 2025, Volume 31 Issue 05
    Stable Tungsten Isotope Composition of Hydrothermal Sediments and Its Implications for the Oceanic Tungsten Cycle
    LIU Shu, HU Rong, LI Tao, YANG Ruiyu, LI Gaojun
    2025, 31(05):  515-523.  DOI: 10.16108/j.issn1006-7493.2024071
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    Stable tungsten isotopes (δ186/184W) are a promising new geochemical proxy for tracing surface material cycles and reconstructing ancient ocean environments. A clear understanding of the source-sink system of stable W isotopes in the ocean is essential for expanding the application. Research indicates that riverine input constitutes the primary source of W in modern oceans, while non-euxinic sediments serve as the main sink. However, the fluxes and isotopic characteristics of different types of non-euxinic sediment sinks remain unclear. Hydrothermal sediments, enriched in hydrothermal sourced iron-manganese oxides, can adsorb significant amounts of W from seawater during sedimentation, resulting in authigenic W enrichment and making them a potentially significant sink. This study analyzed hydrothermal sediment samples from ODP Site 834A in the Lau Basin, South Pacific, to estimate the contribution of hydrothermal sediments to the global oceanic W budget. The high W/ Th in the samples suggests minimal detrital input, while the W/Mo ratio, rare earth element distributions, and δ186/184W values indicate that W in the sediments was primarily adsorbed from seawater by iron-manganese oxides, with manganese oxides playing
    a dominant role. The lower-than-expected isotopic fractionation between sediments and seawater may reflect porewater effects driven by rapid sedimentation and high depositional flux. Based on the W/Mn ratios and global hydrothermal Mn fluxes, the hydrothermal sediments W sink flux is estimated to constitute less than 5% of the total riverine input, implying the presence of other unrecognized major W sinks. 
    Three-dimensional Structure and Velocity Model of Xiaoyangkou Geothermal Field in the Subei Basin
    LIANG Boyu, WANG Maomao, QIAN Jiawei, YU Pengfei, LI Han, ZHANG Chao, YAN Bing, SU Jinbao, MA Haoran
    2025, 31(05):  524-534.  DOI: 10.16108/j.issn1006-7493.2024074
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    The Xiaoyangkou geothermal field is located in the southern part of the Haian sag in the Subei Basin, bounded by
    the near east-west Benchahe fault and the northeast-oriented Jintan-Rugao fault. The geothermal well RRY1 of Xiaoyangkou is currently the only intermediate-temperature geothermal well in Jiangsu Province, with a peak temperature of 92 ℃ . However, the formation, distribution, and relationship of this geothermal resource with the regional fault system remain unclear. This study integrates regional seismic reflection profiles and drilling data to conduct 3D structural and velocity modeling of the Benchahe fault and Jintan-Rugao fault to explore the structural controls on the formation of the Xiaoyangkou geothermal resources. We collected ambient noise data using a dense array and applied cross-correlation calculations, dispersion curve extraction, and direct inversion tomography to construct a 3D shear wave velocity structure down to 4 km. The 3D structural model shows that the Benchahe and Jintan-Rugao faults trend NEE with a northern dip of 60° to 70°. The 3D velocity model reveals significant lateral heterogeneity in the shear wave velocity structure at depths of 2.0 to 3.5 km, with high-velocity and low-velocity boundaries correlating strongly with the Benchahe and Jintan-Rugao faults, reflecting the influence of normal faulting within the sag on the velocity structure. Additionally, a distinct low-velocity anomaly is observed between the Benchahe fault and Jintan-Rugao fault, manifesting vertically as a decrease in shear wave velocity gradient, which coincides with the position of the Silurian quartz sandstone geothermal reservoir at depths of 2.0 to 2.8 km. Based on the regional 3D fault structure and velocity models, as well as previous studies, this research proposes two geothermal modes:‘conductive’above and‘convective’below the Neogene base are primarily controlled by the regional fault system and deep fluid convection, offering a framework for future exploration of faultrelated geothermal resources in coastal zones. 
    Slope Factor Screening and Susceptibility Assessment Based on the Grey Relational Degree Model and Geographic Detector
    XIE Xianjian, Wu Han, Xu Bin, LYU Yiwei
    2025, 31(05):  535-551.  DOI: 10.16108/j.issn1006-7493.2024073
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    Slope factor screening and susceptibility assessment play a significant role in reducing landslide disaster risks, optimizing land use, protecting ecological environments, advancing scientific research, and enhancing governmental disaster management capabilities. This study first constructs a landslide susceptibility database considering two aspects: terrain and basic geological factors, as well as hydrological environment, surface cover, and socioeconomic factors. Then, utilizing GIS technology, it employs principal component analysis, grey relational analysis, geographic detector methods, and the coefficient of variations to diagnose the critical factors influencing landslide susceptibility in the Xiaojiang River Basin. In addition, it uses the weighted overlay tool in spatial analysis to conduct a comprehensive assessment of landslide susceptibility in the study area. The results indicate that the area proportions of extremely high, high, moderate, low, and extremely low susceptibility zones in the study area are 9.91:21.90:29.76:26.00:12.43, respectively. Verification was conducted on 176 different grades of landslide types in the study area, and 75.76% of the total number of large and mega-sized landslides are distributed within the high and extremely high susceptibility zones, which together cover 31.81% of the basin’s total area. Small and medium-sized landslides are entirely distributed in the moderate, low, and extremely low susceptibility zones, with few large and mega-sized landslides found in the low and extremely low susceptibility areas. The evaluation of landslide susceptibility using 15 critical factors, selected by the grey relational analysis model and the geographic detector method, agrees with the real-world conditions. This confirms the accuracy of the methods and can provide a scientific basis for landslide susceptibility assessment in the study area.
    Study on the Temperature Distribution Characteristics and Its Influencing Factors of Granite under Microwave Surface Irradiation
    LONG Yangwei, ZHAO Xiaobao, ZHU Feng, MA Zhongjun
    2025, 31(05):  552-561.  DOI: 10.16108/j.issn1006-7493.2024082
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    The essence of microwave-weakening rocks is thermal destruction. Accurately understanding the temperature distribution characteristics of rocks under microwave irradiation is of great importance for indicating the extent and degree of microwave weakening of rocks. In this paper, the numerical model was first calibrated through experiments, and then the temperature distribution characteristics of granite under microwave surface irradiation were studied using the calibrated numerical model. The influence of irradiation distance, tilt angle, and antenna type on the temperature distribution characteristics (surface maximum temperature rise, shape and size of the high-temperature zone and the influence zone) of rocks was also discussed. The research results show that the surface temperature rise of rocks is symmetrical around the center point and gradually decreases from the center to the edge, and the surface maximum temperature rise of rocks decreases with the increase of irradiation distance and rock tilt angle. The surface maximum temperature rise of microwave-treated rock using the converging waveguide antenna irradiation is 1.35 times that of the standard waveguide antenna, but it gradually decreases as the irradiation distance increases and ultimately lower than that of the standard waveguide antenna. The high-temperature zone on the rock surface is approximately circular when the irradiation distance and tilt angle are zero, and the shape of the high-temperature zone changes with the change of irradiation distance, tilt angle, and antenna type. The surface size and depth of the high-temperature zone are negatively correlated with the irradiation distance and tilt angle and the cross-sectional size of the high-temperature zone decreases gradually with depth until it disappears. Similarly, the surface influence zone of rocks is approximately circular when the irradiation distance and tilt angle are zero, and it also changes with the change of irradiation distance, tilt angle, and antenna type. The surface size of the influence zone is positively correlated with the irradiation distance and tilt angle, and the cross-sectional size of the influence zone initially increases and then decreases with increasing rock depth.
    MICP Based Bio-healing Method for Non-penetrating Steep Rock Fractures with High Bridging Rate
    DAI Qichen, PAN Xiaohua, ZHANG Yichen, TANG Chaosheng
    2025, 31(05):  562-571.  DOI: 10.16108/j.issn1006-7493.2024076
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    Rock instability is a common geological hazard in human activities, engineering construction, and natural environments. Its widespread and frequent occurrence highlights the urgent need for effective prevention. Both academic and engineering communities generally agree that fracture is a dominant factor controlling rock stability, and healing of shallow fractures with small aperture to prevent further expansion is an effective and economical strategy for actively prevention of rock instability hazards. This study focuses on studying the non-penetrating steep rock fractures with small aperture, and adopts microbialinduced calcium carbonate precipitation (MICP) as the bio-healing technique. A MICP based bio-healing method for nonpenetrating steep rock fractures with high bridging rate was proposed based on an innovative three-step injection strategy. The feasibility of the method was systematically examined through a series of laboratory bio-healing tests, spatiotemporal evolution characteristic tracking of the bio-healing process, testing of physical and mechanical properties, and analysis of typical local microstructures. The regulation laws of key factors affecting the bio-healing effect were identified, the microstructural evolution characteristics and the optimal combination scheme of influencing factors for each treatment step was determined.
    Study on Strength and Deformation Characteristics of Cement Loess Improved with Three Forms of Fiber
    HUO Kaizhi, XIE Wanli, MA Chen, ZHANG Jiahao, GAO Xuanyu, DI Shengjie, ZHANG Ying, LIU Xiaomin
    2025, 31(05):  572-581.  DOI: 10.16108/j.issn1006-7493.2024078
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    To investigate the influence of fiber forms on the strength and deformation characteristics of cement loess, the cement loess mixed with three different types of polypropylene fiber (bunched monofilament fiber, mesh fiber, and stranded fiber) was studied by direct shear, static triaxial and SEM tests. The experimental results show that: (1) the addition of three kinds of fibers can effectively improve the shear strength and cohesion of cement loess, and the cohesion of three kinds of soils increases first and then decreases with the increase of the content of dimension. The optimal content of stranded, reticulated and bunched monofilament fibers is 0.3%, 0.35% and 0.55%. (2) The strength and deformation characteristics of modified cement loess with stranded fiber and mesh fiber are different in direct shear test and triaxial test. (3) The three-dimensional network structure of the network fiber can effectively restrain soil deformation and improve soil strength in the triaxial test; The strong deformation resistance of the stranded fiber can play a good role in the direct shear test. (4) The interfacial friction between fiber and soil plays an important role in the improvement of cement loess with three kinds of fibers. Stranded fibers mainly improve soil strength through their good resistance to deformation. 
    Characteristics of Pore Evolution during Hydrocarbon Generation in Shales of Different Lithologies in the Dongying Depression
    ZHANG Xi, YAO Suping, LI Junliang, LIU Yang, XU Chang, LU Xiao
    2025, 31(05):  582-593.  DOI: 10.16108/j.issn1006-7493.2024079
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    The state and content of oil and gas in shale are closely related to the shale reservoir pores, and the complex size of
    the reservoir pore network in shale is between the nanometer and micrometer levels, which is jointly influenced by multiple factors such as hydrocarbon evolution, hydrocarbon forming organism types, and the combination of mineral and organic matter characteristics. In this paper, we take the combined shale of multi-algal-type symbiotic muddy texture-microcrystalline gray texture in the Fengye 1-1HF well of the Minfeng Depression of the Dongying Depression and the combined shale of cyanobacterial algal mat muddy texture-microcrystalline gray texture in the Niuzhuang Depression Niuye 2HF well of the Niuzhuang Depression as the objects of our study. Thermal simulation experiments, pyrolysis, organic carbon mass fraction, specular plasma reflectivity, whole-rock X-ray diffraction, scanning electron microscopy,nuclear magnetic resonance cryoporomety and other analytical tests were utilized to reveal the evolutionary characteristics of reservoir pores during hydrocarbon production in shales of different lithological types. The results show that there are differences in the hydrocarbon generation process and pore development and evolution characteristics of shales in different lithologies. The oil generation window of the sample from the Fengye 1-1HF well is wide, and a large number of organic matter cavities and clay mineral intergranular pores are developed in the mud grain layer of the multi-algal symbiosis, and microcrystalline intergranular pores are developed in the gray grain layer. There are two peaks of hydrocarbon production in the samples from the Niuye 2HF well, the clay mineral intergranular pores are mainly developed in the cyanobacterial algal mat muddy texture layer, and the gray texture layer of gravelly algal gravel is tightly stacked, with poorly developed pores. The transformation of clay minerals during hydrocarbon production and the dissolution and reprecipitation of alkaline minerals have important effects on the pore modification of shale reservoirs. 

    Decollement Deformation Characteristics and Genesis Analysis of Xinglong Tectonic Belt in Linhe Depression of Hetao Basin: Insight from Sand Box Simulation Experiments
    WU Xi, LIU Xin, LIU Xiheng, DAN Weining, LIU Jing, LI Xiao dong, WU Han, YU Zhanwen, TIAN Sisi, YU Fusheng
    2025, 31(05):  594-608.  DOI: 10.16108/j.issn1006-7493.2024072
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    The Xinglong structural belt is located in the northwest of Linhe depression in Hetao Basin. The exploration results of Well Hetan 101 with a daily oil production of 1000 tons prove that the structural belt has great potential for resource exploration. However, the poor understanding of the main controlling factors of the genesis of the oil and gas anticline structure impedes the implementation of the ultra-deep risk exploration well location deployment plan. Based on the refined interpretation of 3D seismic data in the study area, combined with the structural analysis, balanced section analysis and physical simulation of structures, this paper investigates the deformation characteristics and genetic mechanism of the detachment structure. The results show that: (1) The Xinglong tectonic belt experienced the evolution stages of compression depression, tension-shear fault depression and strike-slip transformation. The preexisting thrust faults of the basement formed in the compression stage control the initial development position of the detachment structure, and the spatial distribution characteristics of the gypsum rock layer control the development range of the cap rock detachment structure. (2) with the influence of pre-existing structure and sedimentary environment changes, salt lakes continued to migrate northward and shrink, resulting in significantly different spatial distribution characteristics of the gypsum rock detachment layer, which in turn leads to different structural styles of the detachment faults along the strike. (3) The detachment layer exerts a significant decoupling effect. The detachment layer causes a significantly different structural deformation pattern on and below the salt. The increase in the detachment layer thickness would enhance its decoupling effect. The enhanced decoupling effect reduces the number of detachment faults, increases the horizontal detachment distance, and increases the size of a single detachment system. In addition, secondary faults are developed near the main detachment fault and areas away from the main detachment fault, the. (4) Under the extension regime, the detachment transfer mode of progressive deformation with the main detachment fault to the front will occur above the ductile detachment layer, and the amplitude and size of anticline decrease in turn. When the tensile stress on both sides is equal and the thickness of the detachment layer is same, the transmission distance of the deformation fronts on both sides of the model tends to be consistent, showing characteristics of symmetrical deformation.
    Indicative Significance of Oil Biodegradation in Petroleum Accumulation of the Shunbei Oilfield,Tarim Basin
    ZHU Lianhua, ZHANG Qian, BU Xuqiang, LI Meijun, QIAO Rongzhen, ZHANG Donglin, XIAO Hong
    2025, 31(05):  609-617.  DOI: 10.16108/j.issn1006-7493.2024075
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    In the context of ultra-deep oil, biodegradation is often regarded as a secondary process. The detection of 25-norhopane compounds in ultra-deep oil from the Shunbei oilfield presents an opportunity to explore the role of biodegradation in ultradeep petroleum accumulation. This study analyzes petroleum geochemistry and accumulation using gas chromatographymass spectrometry, carbon isotope analysis, fluid inclusion analysis, single-well burial-thermal history, and thermal evolution simulations of source rocks. Gas chromatography, mass spectrometry, and carbon isotope analyses indicate that the oil in the Shunbei oilfield belongs to the same oil family. The oil exhibits high maturity, and the source rocks were formed in a weakly oxidizing-reducing environment with marine Type II or Ⅱ / Ⅲ organic matter as the primary contributor. Fluid inclusion and burialthermal history analyses reveal two primary periods of oil charging in the study area: the Late Caledonian and Indosinian periods. The detection of 25-norhopane compounds and complete n-alkanes in the crude oil further supports the occurrence of these two distinct oil charging periods. The integration of burial-thermal history with petroleum charging time suggests that the oil is predominantly a mixture of biodegraded oil from the Late Caledonian period and fresh oil from the Indosinian period. Therefore, biodegradation plays a crucial role in understanding the hydrocarbon accumulation processes in the Shunbei oilfield.
    Characteristics and Genetic Mechanism of Present-day Geothermal Field in Western Junggar Basin
    XU Jiabo1, 2, 3, CHANG Jian1, 2, 3, GUO Huajun4, LI Chenxing2, 3, SHAN Xiang4, PENG Bo4, QIU Nansheng2, 3, ZHANG Ze2, 3
    2025, 31(05):  618-631.  DOI: 10.16108/j.issn1006-7493.2024083
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    This study explores the geothermal features of the Mahu Sag and Ke-Wu fault zone, including the present-day
    geothermal gradient, terrestrial heat flow, formation temperatures at depths of 5000-8000 m, and the lithosphere’s thermal structure, utilizing data from 70 wells and 98 rock samples, and establishes a geothermal genetic model for the Mahu-Ke-Wu region. In the Mahu-Karamay-Wuerhe region, the thermal conductivity of Carboniferous-Paleogene rocks ranges from 1.5 to 3.03 W/(m·K), exhibiting a stepwise increase with the age of the strata. The geothermal gradient in the study area ranges from 16.25 to 22.42 ℃ /km (Avg: 21.18 ℃ /km). The heat flow ranges from 34.73 to 52.62 mW/m2 (Avg: 44.01 mW/m2). The temperature of strata at 5000 meters depth ranges from 85.4 to 126.5 ℃ (Avg:113.2 ℃). At 6000 meters depth, the temperature ranges from 104.9 to 144.2 ℃ (Avg: 134.9 ℃). At 7000 meters depth, the temperature ranges from 120.9 to 167.9 ℃ (Avg: 153.6 ℃). At 8000 meters depth, the temperature ranges from 133.8 to 182.3 ℃ (Avg: 170.8 ℃). Vertically, the geothermal gradient decreases by 2 ℃ /km. The heat flow ratio between the fault zone and the sag crust-mantle is 0.77 and 1.20, respectively, indicating a typical cold crust and cold mantle structure. The geothermal genetic model of the Mahu-Karamay-Wuerhe region shows that the crustal structure of different tectonic units, along with variations in thermal conductivity between the sedimentary cover and the folded basement rocks, is the key factor governing the distribution of the geothermal field in the study area. The varying depths of the Moho surface in the sag and fault zones provide different amounts of heat to the surface, and the differences in rock thermal conductivity allows redistribution of heat in the shallow strata, resulting in a convex high-concave low heat flow distribution pattern.
    Need for Critical Metals in the Development of Carbon-neutral Technologies
    ZHOU Yiyang, ZHAO Liang, ZHU Chen, ZHANG Menglong, FENG Henan, SUN Jiajia
    2025, 31(05):  632-645.  DOI: 10.16108/j.issn1006-7493.2024044
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    With the deepening of global attention to climate change, carbon neutrality has become a general consensus and
    strategic goal of the international community. Achieving this goal relies on a wide range of advanced technologies and solutions, including renewable energy, electric vehicles, energy storage systems, and carbon capture, utilization and storage (CCUS) technologies. However, the large-scale deployment of these technologies has created a surge in demand for key metals, posing a new challenge. This paper reviews the dynamic changes in the demand for key metals in the context of the development of carbon neutral technologies, explores the potential supply risks, and proposes countermeasures. This paper analyzes the dependence of key technologies such as wind energy, solar photovoltaic, battery energy storage, hydrogen energy and electric vehicles on key metals such as lithium, cobalt, nickel and rare earth elements. With the rapid growth of installed clean energy capacity, the demand for these metals is expected to rise significantly in the coming decades. For example, demand for lithium, cobalt and nickel for electric vehicle batteries and for rare earth metals such as neodymium and dysprosium used in wind turbine magnets is growing far faster than current mining and recycling capabilities. In conclusion, the rapid development of carbon-neutral technologies poses new challenges to the demand for key metals, requiring a global vision and innovative solutions to ensure sustainable supply of resources and support the global transition to a low-carbon economy.