- Geological and Geochemical Analysis
- earthquake and tectonic studies
- High-pressure geophysics and materials
- Geochemistry and Geologic Mapping
- Geological and Geophysical Studies
- Geochemistry and Geochronology of Asian Mineral Deposits
- Geological Studies and Exploration
- Geochemistry and Elemental Analysis
- Paleontology and Stratigraphy of Fossils
- Hydrocarbon exploration and reservoir analysis
- Geology and Paleoclimatology Research
- Underwater Acoustics Research
- Underwater Vehicles and Communication Systems
- Electrochemical Analysis and Applications
- Paleontology and Evolutionary Biology
Sun Yat-sen University
2016-2024
Institute of Tibetan Plateau Research
2024
Chinese Academy of Sciences
2010-2024
Southern Marine Science and Engineering Guangdong Laboratory (Zhuhai)
2019-2023
Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou)
2019-2023
Peking University
2017
University of Hong Kong
2007-2014
Institute of Geology and Geophysics
2010-2014
University of Waterloo
2012-2014
Hong Kong University of Science and Technology
2007-2011
The evolution of South China involved accretion-collision multiple terranes from the Proterozoic to Mesozoic.Zircon U-Pb ages, Hf data, and structural data indicate that Cathaysia block consists two terranes, West East Cathaysia, separated by a newly recognized major strike-slip fault.We propose was part microcontinent originated Grenvillian-aged orogen in Rodinia supercontinent, an Indosinian-aged Paleo-Tethyan regime south translated east through motion, early Paleozoic Wuyi-Yunkai orogeny...
This paper presents petrographic and mineral chemistry data an inferred P-T path for the high-pressure pelitic granulites from Helanshan Complex in Khondalite Belt, a Palaeoproterozoic collisional belt along which Yinshan Ordos blocks joined to form Western Block North China Craton. Petrographic observation indicates that these experienced four metamorphic stages: early prograde (M~1~), peak (M~2~), post-peak decompression (M~3~) late retrograde (M~4~) stages. The assemblage (M~1~) is...