A5085279961- Geological and Geochemical Analysis
- Geochemistry and Geologic Mapping
- earthquake and tectonic studies
- High-pressure geophysics and materials
- Geochemistry and Geochronology of Asian Mineral Deposits
- Geological and Geophysical Studies
- Geochemistry and Elemental Analysis
- Geology and Paleoclimatology Research
- Paleontology and Stratigraphy of Fossils
- Hydrocarbon exploration and reservoir analysis
- Geological Studies and Exploration
- Methane Hydrates and Related Phenomena
- Metal Extraction and Bioleaching
- Metallurgy and Cultural Artifacts
- Marine and environmental studies
- Radioactive element chemistry and processing
- Minerals Flotation and Separation Techniques
- Hydraulic Fracturing and Reservoir Analysis
- Geomagnetism and Paleomagnetism Studies
- Metallurgy and Material Science
- Linguistics and language evolution
- Mining and Gasification Technologies
- Advanced machining processes and optimization
- Mineralogy and Gemology Studies
China University of Geosciences (Beijing)
2015-2024
Xinjiang Institute of Ecology and Geography
2024
Chinese Academy of Sciences
2024
Beijing Institute of Geology for Mineral Resources
2024
Nanjing University
2021-2022
Natural History Museum
2019-2022
University of Exeter
2022
Bureau of Geology and Mineral Exploration and Development of Guizhou Province
2021
China University of Petroleum, Beijing
2013
Abstract Situated in the heart of Tien Shan gold province, Unkurtash (3.5 Moz at 1.82 g/t) is a representative lode deposit that hosted within Carboniferous Andagul granodiorite Kassan district, western Kyrgyzstan. The province consists porphyry and epithermal deposits, which are related to magmatic arcs, deposits formed late stages continent-continent collision have been generally classified as mesothermal or orogenic type. Some considered be intrusion-related, but genetic relationship...
The Halasu area is located in the southeastern margin of Chinese Altai Xinjiang, China. It part Altaid orogenic collage where a number porphyry-type Cu–Mo–Au deposits have been discovered recent years. Geological mapping and drilling indicate presence various mineralized porphyritic intrusions Cu–Au deposit, which currently under exploration. U–Pb dating zircon crystals from four different porphyries reveals three significantly ages magmatic intrusion, i.e., ca. 372–382 Ma granodioritic...
To understand the orogenic cyclicity that built northern Yili magmatic arc in southern Balhkash-Yili of Central Asian Orogenic Belt, we synthesize its tectono-magmatic processes using new and existing U-Pb geochronological dates (228), Hf-in-zircon (1605 spots), bulk-rock geochemical data (1458), Sr-Nd isotopic analyses (461) rocks. Based on temporal-spatial distribution rocks their composition, four episodes (ca. 470−440 Ma, 420−380 350−320 300−260 Ma) punctuated by a gap 440−420 two...
Constructing the plutonic–volcanic connections in volcanic arc setting is essential for understanding a variety of magmatic processes from continental crust differentiation to formation magmatic‐hydrothermal ore deposits. Based on combination zircon U–Pb geochronology and Hf isotope whole‐rock geochemistry Sr‐Nd isotopes, we evaluated potential between plutonic rocks Tulasu Basin, largest epithermal gold district Chinese Western Tianshan. The peak volcanism coincides well with major...
Separation of Au and Sb mineralization from different hydrothermal stages is a common phenomenon in many Au–Sb deposits, but its cause remains enigmatic. The Qukulekedong intrusion-related deposit the East Kunlun Orogen has undergone four stages: (1) barren quartz vein, (2) vein with disseminated arsenopyrite–pyrite alteration halo, (3) stibnite–quartz ± native gold (4) calcite–quartz vein. Stages 2 3 formed vein-type ore, respectively. Here, internal texture trace elements quartz, fluid...