A5077604367- Geological and Geochemical Analysis
- High-pressure geophysics and materials
- earthquake and tectonic studies
- Geological and Geophysical Studies
- Geochemistry and Geologic Mapping
- Hydrocarbon exploration and reservoir analysis
- Particle physics theoretical and experimental studies
- Paleontology and Stratigraphy of Fossils
- Quantum Chromodynamics and Particle Interactions
- High-Energy Particle Collisions Research
- Geological Studies and Exploration
- Methane Hydrates and Related Phenomena
- China's Ethnic Minorities and Relations
- Geochemistry and Elemental Analysis
- Seismic Imaging and Inversion Techniques
- Geochemistry and Geochronology of Asian Mineral Deposits
- Geological formations and processes
- Chinese history and philosophy
- Global Trade and Competitiveness
- Building materials and conservation
- Geology and Paleoclimatology Research
- Seismic Waves and Analysis
- Healthcare Policy and Management
- Context-Aware Activity Recognition Systems
- Microbial bioremediation and biosurfactants
China University of Geosciences
2014-2024
State Key Laboratory of Geological Processes and Mineral Resources
2024
Guangzhou Institute of Geochemistry
2014-2023
Chinese Academy of Sciences
2014-2023
Tongji University
2019-2023
Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou)
2022
China Earthquake Administration
2022
China University of Geosciences (Beijing)
2021
Army Medical University
2017
Daping Hospital
2017
High-precision U-Pb zircon ages of 125.755 ± 0.061 Ma and 124.122 0.048 Ma, respectively, represent the onset termination Yixian Formation in Jin-Yang basin, bracketing its duration to 1.633 0.078 Myr.
The 2022 MS 6.8 Luding earthquake is the strongest in Sichuan Province, Western China, since 2017 7.0 Jiuzhaigou earthquake. It occurred on Moxi fault southeastern segment of Xianshuihe fault, a tectonically active and mountainous region with severe secondary disasters. To better understand seismogenic mechanism provide scientific support for future hazard mitigation, we summarize preliminary results earthquake, including seismotectonic background, seismicity mainshock source characteristics...
Taking the Permian Lucaogou Formation in Malang sag, Santanghu Basin as an example, by using petrological methods such high resolution core image scanning, conventional thin section, scanning electron microscope and energy spectrum analysis geochemical tests trace elements biomarker compounds, petrologic features sedimentary origin of lamellar organic rich fine-grained rocks lake facies were investigated, its significance for shale oil tight exploration was analyzed. The results study show...
Early Paleozoic amphibolite- to granulite-facies metamorphism, crustal anatexis and coeval magmatism are extensively developed in the Wuyi–Yunkai intraplate orogen South China block. However, exact timing of partial melting its link with orogenesis have not been well constrained. In this study, charnockites, gneissic migmatites Al-rich gneisses (Grt–Sil–Bt gneiss Bt–Pl gneiss) from Gaozhou Complex Yunkai uplift Cathaysia block were selected for analysis whole-rock major elements zircon U–Pb...
High-Mg andesites (HMAs) and adakitic rocks are purported to occur exclusively in subduction zones the modern Earth. In North China Craton, early Cretaceous HMAs dacites were erupted a continental setting, apparently unrelated given their location distal (>1000 km) trench at that time. Here we report petrological, mineralogical geochemical data for these with aim of constraining petrogenesis elucidating role water intraplate magmatism cratonic destruction. The can be subdivided into olivine...
Abstract 809 deep IODP Hole U1473A at Atlantis Bank, SWIR, is 2.2 km from 1,508‐m 735B and 1.4 158‐m 1105A. With mapping, it provides the first 3‐D view of upper levels a 660‐km 2 lower crustal batholith. It laterally vertically zoned, representing complex interplay cyclic intrusion, ongoing deformation, with kilometer‐scale upward lateral migration interstial melt. Transform wall dives over gabbro‐peridotite contact found only evolved gabbro intruded directly into mantle near transform....
Abstract Subduction of the paleo-Pacific plate during late Mesozoic is thought to have been responsible for destruction North China craton, manifested by intense volcanism, lithospheric deformation, and dramatic changes in surface morphology terrestrial ecosystems. However, timing correlations these consequential events remain obscure. This issue was addressed here carrying out a high-resolution geochronologic study on Upper Jurassic–Lower Cretaceous sequences Luanping basin, northern Hebei...