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中国地质(英文)
中国地质(英文)

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2096-5192

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100037

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中国地质(英文)/Journal China GeologyCSTPCDCSCD北大核心
查看更多>>本刊旨在围绕地球多圈层交互作用调查研究、能源和其他重要矿产资源调查评价、水文地质与水资源调查评价、山水林田湖草综合调查评价与生态保护修复、海洋地质调查、重要经济区与城市地质调查评价、国际地质合作研究等方面,与世界各国同行交流地质科学研究新问题和地质调查新发现,传播地质新理念,共同探讨信息化、网络化、数字化背景下,地质工作如何保持先行者的形象,持续高效地支撑全球经济发展和环境保护。依托中国地质调查创新发现的优势,设立原创性学术论文、综述性学术论文、最新研究进展、地质界简讯与新闻等四大栏目,重点刊发在解决重大资源环境和基础地质问题过程中前瞻性、引领性、颠覆性学术成果;重点刊发基础性、综合性、专题性综述性成果;重点刊发最新发现和最新地质调查数据等优秀成果。
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    Application of geophysical methods in fine detection of urban concealed karst:A case study of Wuhan City,China

    Dao-han LiuLei WangLei LiuJun-jie Xu...
    517-532页
    查看更多>>摘要:The construction of modem livable cities faces challenges in karst areas,including ground collapse and engineering problems.Wuhan,with a population of 13.74×106 and approximately 1161 km2 of soluble rocks in the urban area of 8569.15 km2,predominantly consists of concealed karst areas where occasional ground collapse events occur,posing significant threats to underground engineering projects.To address these challenges,a comprehensive geological survey was conducted in Wuhan,focusing on major karst-related issues.Geophysical methods offer advantages over drilling in detecting concealed karst areas due to their efficiency,non-destructiveness,and flexibility.This paper reviewed the karst geological characteristics in Wuhan and the geophysical exploration methods for karst,selected eight effective geophysical methods for field experimentation,evaluated their suitability,and proposed method combinations for different karst scenarios.The results show that different geophysical methods have varying applicability for karst detection in Wuhan,and combining multiple methods enhances detection effectiveness.The specific recommendations for method combinations provided in this study serve as a valuable reference for karst detection in Wuhan.

    Geology and mineralization of the Dongping supergiant alkalic-hosted Au-Te deposit(>100t Au)in Northern Hebei Province,China:A review

    Shi-min ZhenDa-zhao WangZhong-jian ZhaHai-jun Bai...
    533-550页
    查看更多>>摘要:The Dongping deposit is the largest alkalic-hosted gold deposit in China containing>100 t of Au.This paper presents a new understanding for Dongping ore system,based on the previous studies.The mineralization originally occurred at 400-380 Ma,simultaneous with emplacement of the Shuiquangou alkaline complex,and was overprinted by the hydrothermal activity in the Yanshanian.Isotope compositions of ores indicate metals of the deposit are mainly provided by the Shuiquangou complex.Ore-forming fluids are characterized by increasing oxygen fugacity and decreasing sulfur fugacity,while tellurium fugacity increased in the Stage Ⅱ-2 and decreased in Stage Ⅱ-3.These systematic changes are closely related to the processes of mineral precipitation and fluid evolution.Sulfide precipitation from Stage I to Stage Ⅱ was triggered by fluid boiling,which leads to the precipitation of Pb-Bi-Te,due to decrement of sulfur fugacity.Condensation of gas phase containing high concentration of H2Te leads to precipitation of Te-Au-Ag minerals and native tellurium.Based on these hypotheses,this paper present a polyphase metallogenic model as follow.During the Devonian,fluids were released from alkaline magmas,which carried ore-forming materials form the surrounding rocks and precipitate the early ores.During the Jurassic-Cretaceous,fluorine-rich fluids exsolved from highly factionated Shangshuiquan granite,which extracted and concentrated Au from the Shuiquangou complex and the Sanggan Group metamorphic rocks,and finally formed the Dongping gold deposit.

    Formation,evolution,reconstruction of black shales and their influence on shale oil and gas resource

    Shi-zhen LiQiu-chen XuMu LiuGuo-heng Liu...
    551-585页
    查看更多>>摘要:Black shales are important products of material cycling and energy exchange among the lithosphere,atmosphere,hydrosphere,and biosphere.They are widely distributed throughout geological history and provide essential energy and mineral resources for the development of human society.They also record the evolution process of the earth and improve the understanding of the earth.This review focuses on the diagenesis and formation mechanisms of black shales sedimentation,composition,evolution,and reconstruction,which have had a significant impact on the formation and enrichment of shale oil and gas.In terms of sedimentary environment,black shales can be classified into three types:Marine,terrestrial,and marine-terrestrial transitional facies.The formation processes include mechanisms such as eolian input,hypopycnal flow,gravity-driven and offshore bottom currents.From a geological perspective,the formation of black shales is often closely related to global or regional major geological events.The enrichment of organic matter is generally the result of the interaction and coupling of several factors such as primary productivity,water redox condition,and sedimentation rate.In terms of evolution,black shales have undergone diagenetic evolution of inorganic minerals,thermal evolution of organic matter and hydrocarbon generation,interactions between organic matter and inorganic minerals,and pore evolution.In terms of reconstruction,the effects of fold deformation,uplift and erosion,and fracturing have changed the stress state of black shale reservoirs,thereby having a significant impact on the pore structure.Fluid activity promotes the formation of veins,and have changed the material composition,stress structure,and reservoir properties of black shales.Regarding resource effects,the deposition of black shales is fundamental for shale oil and gas resources,the evolution of black shales promotes the shale oil and gas formation and storage,and the reconstruction of black shales would have caused the heterogeneous distribution of oil and gas in shales.Exploring the formation mechanisms and interactions of black shales at different scales is a key to in-depth research on shale formation and evolution,as well as the key to revealing the mechanism controlling shale oil and gas accumulation.The present records can reveal how these processes worked in geological history,and improve our understanding of the coupling mechanisms among regional geological events,black shales evolution,and shale oil and gas formation and enrichment.

    Discovery of scheelite in the Zaozigou gold deposit of West Qinling Orogen,Northwest China and its implications for ore genesis

    Meng-xu GuoJia-jun LiuDe-gao ZhaiGuo-ming Weng...
    586-588页

    Muscovite 40Ar/39Ar isotopic dating of pegmatite veins in the Bieyesamas rare metal deposit in the Altay Mountain,Xinjiang,northwestern China

    Geng-biao QiaoPing WangXiao-hong WangJun-lu Chen...
    589-591页

    U-Pb dating of monazite in the Bainiuchang silver polymetallic deposit,Yunnan Province,and its limitation on Mesozoic mineralization

    Bo-de LuWen-chang LiXue-long LiuGuang-zhi Meng...
    592-595页

    Desert ecological control and ecological industrial construction:Practice and inspiration from China

    Xue-zheng GaoLu LiuYun-tao ShangFan-yu Qi...
    596-600页

    Guidelines for Authors

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