A5100461000- Geological and Geochemical Analysis
- earthquake and tectonic studies
- Paleontology and Stratigraphy of Fossils
- High-pressure geophysics and materials
- Geochemistry and Geologic Mapping
- Geological and Geophysical Studies
- Geochemistry and Elemental Analysis
- Paleontology and Evolutionary Biology
- Geological Studies and Exploration
- Marine Biology and Ecology Research
- Geology and Paleoclimatology Research
- Graphene and Nanomaterials Applications
- Barrier Structure and Function Studies
- Anodic Oxide Films and Nanostructures
- Cancer-related gene regulation
- Water Treatment and Disinfection
- Web visibility and informetrics
- nanoparticles nucleation surface interactions
- Geological and Geophysical Studies Worldwide
- Intracranial Aneurysms: Treatment and Complications
- Land Use and Ecosystem Services
- Geological formations and processes
- Remote Sensing and Land Use
- Cancer Mechanisms and Therapy
- Membrane Separation Technologies
Guangdong University of Technology
2021-2025
China Geological Survey
2021-2024
Shangdong Agriculture and Engineering University
2023
Institute of Pharmacology
2022
Research Institute of Petroleum Exploration and Development
2020-2022
China National Petroleum Corporation (China)
2020
Chinese Academy of Geological Sciences
2010-2016
China University of Geosciences
2015-2016
Institute of Geology and Geophysics
2000-2014
Chinese Academy of Sciences
2000-2014
The northern Xinjiang of China is a composite orogenic belt in the south central part Altaids formed by subduction‐accretion mainly during Paleozoic. Geochronologic and geochemical data from Paleozoic ophiolites associated assemblages are reported here to place constrains on tectonic evolution this region reconstruct its history, using model plus large‐scale map‐view strike‐slip faulting. Geologic geochronologic review indicates that western eastern Junggar regions tectonically related,...
The West Junggar Metallogenic Belt (WJMB) is located between the Tianshan fault system and Ertix in western part of Central Asian Domain (CAMD). belt features widespread late Palaeozoic granitic plutons, strike-slip faults, porphyry copper orogenic gold deposits. We collected nine molybdenite samples from Baogutu III–IV Cu–Mo deposit Suyunhe Mo–W deposit, 12 granitoid Jiaman, Kangde, Kulumusu, Bieluagaxi, Hatu, Akbastau, Miaoergou, Baogutu, Karamay, Hongshan plutons WJMB. Molybdenite Re–Os...
The Central Asian metallogenic domain (CAMD) is a multi-core system controlled by boundary strike-slip fault systems. Balkhash belt in Kazakhstan, which occur many large and super-large porphyritic Cu–Mo deposits some quartz vein- greisen-type W–Mo deposits, well-known the CAMD. In this paper 11 molybdenite samples from western segment of are selected for Re–Os compositional analyses isotopic dating. Molybdenites Borly porphyry Cu deposit three vein-greisen deposits—East Kounrad, Akshatau...
Crustal deformation occurred widely in the Yanshan tectonic belt, north of North China Craton, and its time mechanism remain as open problems. On basis new structural data 40Ar-39Ar dating on hornblende biotite from rocks a dynamic link between plate interaction is established. Abundant structures Fengning-Longhua fault zone indicate that it transpressional including both strike-slip (dextral) compressional (south-directed) components kinematically conformable to Huade-Chifeng Neimeng Uplift...
ABSTRACT Yunfuconcha bimenta, a new genus and species of bivalve from the Ordovician western Guangdong, China, is described. Its unusual hinge consists palaeotaxodont-like dentition anteriorly heteroconch-like posteriorly. The posterior area exhibits remarkable, broad, deeply inset, concave ligament area, which reminiscent ventrally expanded some Recent fossil lucinoids triangular resilifer in late Palaeozoic crassatellid heteroconchs. Lamellar teeth sockets complete dentition. combination...