A5102714481- Geological and Geochemical Analysis
- earthquake and tectonic studies
- High-pressure geophysics and materials
- Geochemistry and Geologic Mapping
- Geochemistry and Elemental Analysis
- Geological and Geophysical Studies
- Geochemistry and Geochronology of Asian Mineral Deposits
- Paleontology and Stratigraphy of Fossils
- Radioactive element chemistry and processing
- COVID-19 and Mental Health
- Photosynthetic Processes and Mechanisms
- Geological Studies and Exploration
- Healthcare professionals’ stress and burnout
- Health and Well-being Studies
- Plant Gene Expression Analysis
- Plant biochemistry and biosynthesis
- Hydrocarbon exploration and reservoir analysis
Chinese Academy of Geological Sciences
2014-2023
Ministry of Natural Resources
2018-2023
University of Hong Kong
2010-2014
Shanghai Normal University
2012
Hong Kong University of Science and Technology
2011
Peking University
2006-2009
Ministry of Education of the People's Republic of China
2007
High-pressure (HP) mafic granulites in the Jiaobei terrane are composed predominantly of garnet granulites, garnet–hypersthene and amphibolites, they found as irregular lenses or deformed dike swarms within tonalitic–trondhjemitic–granodioritic gneisses granitic gneisses. The HP contain four distinct metamorphic assemblages, which early prograde assemblage (M1) is represented by cores garnets, together with mineral inclusions clinopyxene + plagioclase ± quartz, it formed at 740–770 °C...
Abstract: The Paleoproterozoic Lüliang Metamorphic Complex (PLMC) is situated in the middle segment of western margin Trans‐North China Orogen (TNCO), North Craton (NCC). As most important lithological assemblages southern part PLMC, Guandishan granitoids consist early gneissic tonalities, granodiorites and monzogranites, younger to massive monzogranites. Petrochemical features reveal that tonalities belong medium‐K calc‐alkaline series; monzogranites are transitional from high‐K shoshonite...