A5069828193- Geochemistry and Geologic Mapping
- Geological and Geochemical Analysis
- Hydrocarbon exploration and reservoir analysis
- Geochemistry and Geochronology of Asian Mineral Deposits
- earthquake and tectonic studies
- Geological and Geophysical Studies
- Geoscience and Mining Technology
- Mining Techniques and Economics
- Geochemistry and Elemental Analysis
- Geological Studies and Exploration
- CO2 Sequestration and Geologic Interactions
- Reservoir Engineering and Simulation Methods
- Coal Properties and Utilization
- Rock Mechanics and Modeling
- High-pressure geophysics and materials
- Geophysical and Geoelectrical Methods
- Methane Hydrates and Related Phenomena
- Mineral Processing and Grinding
- Geomagnetism and Paleomagnetism Studies
China Resources (China)
2013-2024
China University of Geosciences (Beijing)
2004-2009
China's largest gold resource is located in the highly endowed northwestern part of Jiaodong province. Most deposits this area are associated with NE- to NNE-trending shear zones on margins 130–126 Ma Guojialing granite. These collectively formed at ca. 120 ± 5 during rapid uplift The Dayingezhuang deposit a large (> t Au) orogenic same area, but along eastern margin Late Jurassic Linglong Metamorphic Core Complex. New 40Ar/39Ar geochronology hydrothermal sericite and muscovite from indicate...
Abstract The Jiapigou gold belt, one of the most important gold‐producing districts in China, is located northern margin North China Craton (NCC). tectonic evolution belt closely related to Siberian Plate (SP) north, Yangtze (YC) south and Pacific east. In order investigate nature tectono‐fluid‐metallogenic system, authors investigated relationships among regimes, fluid metallogenesis. This paper examined corresponding spatial–temporal relationship between ore‐controlling regime hydrothermal...
Abstract The Dayingezhuang gold deposit is located in the central part of Zhaoping Fault Zone, which one most important gold‐hosting faults Jiaodong province China. a typical large‐scale shear zone‐hosted disseminated with superimposed silver mineralization. Fluid inclusion (FI) petrography and microthermometry, analysis oxygen hydrogen isotopes for fluid inclusions were conducted to determine characteristics ore‐forming fluids processes Microthermometry data FI indicated that are...
Over the past two decades, significant deposit discoveries were made in Northeastern China, including super-large Chalukou, Daheishan, and Luming porphyry Mo deposits. The discovery of was accomplished through verification stream sediment anomalies, with mineralization closely associated early Jurassic monzogranite granite porphyry. Previous studies primarily focused on mechanisms these deposits without adequately addressing exploration methods prospecting criteria. This study involved a...
Abstract: During the Paleozoic, Ordos area in western North China Plate was located at intersecting position of microplates and controlled by their interaction. The structural framework area, which underwent transformations Ordovician, Carboniferous Permian respectively, dominated alternation uplift depression. are utilized as clues to investigate microplates' interacting type its response area. According regional evolution, is simplified into an isopachous, isotropic elastic shell model,...
Abstract: The Tongling ore cluster area experienced intensive compression and associated shearing during the Indosinian‐Yanshanian Epoch, which formed a trunk ore‐controlling fold fault system in caprock. magmatic intrusion Yanshanian Epoch induced multi‐stage unmixing of poly‐phase fluids, resulting mineralization characterized by multi‐layer, wide‐range, multiform styles. not only supplied essential ore‐forming materials, but also reconstructed structures according to trend surface...
Abstract Based on the data of field measurement and drilling in Tongling area, a series numerical simulations are carried out by using “Surplus Space Method” (SSM), which is first put forward this paper applied to predict shallow‐seated magmatic bodies. The results show existence 3‐D shape conical structure at depth −1000 m beneath center area: its top offsets southwards bifurcates several branches, while lower part stretches northeastwards contracts rapidly point about depth. This reckoned...
The stated-owned exploration companies (SOEC), of state-owned enterprises background, go for profits as well national and social responsibility. SOEC play significant roles in commercial mineral by taking advantage their brands, strong financial backing operation capability to integrate the capital technology. Since disadvantage backwardness, have deal with multiple problems, such high costs rights acquisition, multi-cooperation project management, criterions traditional techniques can not...