A5102878198- Geological and Geochemical Analysis
- earthquake and tectonic studies
- Geological and Geophysical Studies
- High-pressure geophysics and materials
- Hydrocarbon exploration and reservoir analysis
- Geological formations and processes
- Geochemistry and Geochronology of Asian Mineral Deposits
- Geological Studies and Exploration
- Methane Hydrates and Related Phenomena
- Geochemistry and Geologic Mapping
- Seismic Imaging and Inversion Techniques
- Geology and Paleoclimatology Research
- Optical measurement and interference techniques
- Rock Mechanics and Modeling
- Advanced Photocatalysis Techniques
- Catalytic Processes in Materials Science
- Structural Health Monitoring Techniques
- Radioactive element chemistry and processing
- Paleontology and Stratigraphy of Fossils
- Vibrio bacteria research studies
- Seismology and Earthquake Studies
- Plasma Applications and Diagnostics
- Microbial Fuel Cells and Bioremediation
- CO2 Sequestration and Geologic Interactions
- Geochemistry and Elemental Analysis
Ocean University of China
2014-2025
Zhejiang University of Technology
2024
Qingdao National Laboratory for Marine Science and Technology
2017-2023
Ministry of Education of the People's Republic of China
2011-2016
Ministry of Natural Resources
2016
The East China Sea basins, located in the West Pacific Continental Margin (WPCM) since late Mesozoic, mainly include Shelf Basin (ECSSB) and Okinawa Trough (OT). WPCM its adjacent seas can be tectonically divided into five units from west to east, including Min‐Zhe Uplift, ECSSB, Taiwan–Sinzi Belt, OT, Ryukyu Island Arc, which record regional tectonic evolution geodynamics. Among those units, ECSSB OT are important composite sedimentary pull‐apart experienced two stages of strike‐slip...
Since the Mesozoic, North China Craton has been located at a triangular junction surrounded by subduction or collision zones. This craton thus marks frontier of super‐convergent regime. Within super‐convergence tectonic domains, however, distinct extensional regimes operated in Meso‐Cenozoic Bohai Bay Basin eastern part Craton. In this synthesis, we focus on intracontinental dynamics during Mesozoic to Cenozoic Whereas deep structures as revealed from tomographic studies show remarkable...
Abstract There is a continuing hot debate on whether the geodynamics in West Pacific indicate either marginal basin or back‐arc basin, since nature, evolution and formation mechanism are not well known. Research Okinawa Trough (OT), which an active has important scientific significance for discussing opening development of basin. This paper synthesizes data crustal thickness, heat flow, hydrothermal activity fault patterns to determine geological nature OT. By comparing thicknesses initial...
It is a hot debate on the Meso-Cenozoic dynamics of East Asian continental margins,since nature,type and evolution its margins are not well-known..This paper systematically summarizes results plate reconstructions margin since Permian over past 40 years with emphasis new research in 10 years.The mainly focuses variation types Late Triassic,the transitions among different tectonic domains.Our data suggests that as whole experienced pre-Triassic passive margin,a Triassic-Early Cretaceous...
Abstract The Borneo Accretionary Orogen (BAO) is located in a central position of SE Asia, surrounded by the long‐lived westward subduction Pacific Plate, northward Indian Plate beneath Eurasian and passive continental margin South China Sea. Based on previous studies stratigraphy, structural geology geophysics, number tectonic models BAO have been proposed, but these do not perfectly match all geological facts. A field‐based analysis rocks Sabah Malaysia has recognized that deformation can...
Abstract This article discusses the ‘Power-to-X’ (P2X) concept, highlighting integral role of non-thermal plasma (NTP) in P2X for eco-friendly production chemicals and valuable fuels. NTP with unique thermally non-equilibrium characteristics, enables exotic reactions to occur under ambient conditions. review summarizes plasma-based systems, including discharges, reactor configurations, catalytic or non-catalytic processes, modelling techniques. Especially, potential directly convert stable...
The South China Sea was formed in Cenozoic.Basins the could be divided into different types,such as continental shelf basins,continental slope basins and deep sea basins,which are closely related with rifting transition of margins,and thus grouped strike-slip-related pull-apart extensional basins,extrusion-escape-related basins,extension-and subduction-related buckling basins.They developed further some ridge-spreading-related oceanic sub-basins stages.These were not under a single dynamics...
Abstract The Yangtze foreland fold‐and‐thrust belt is located between the Mesozoic Dabie collisional orogen and Jiangnan intraplate in east‐central China. Three regional deformation events are recognized Orogen north of River. earliest (D1) corresponded to a southeastward compression that occurred during subduction South China Plate below North Plate. Top‐to‐the‐southeast shearing coeval with Late Permian–Early Triassic blueschist facies metamorphism, was possibly associated development...
Paleo- to Mesoproterozoic sedimentary rocks in the southern margin of North China Craton (NCC) are represented by Ruyang and Luoyu groups. We studied from Yunmengshan Beidajian formations Group Cuizhuang Sanjiaotang Group. Detrital zircon grains these have U–Pb age populations 3.64–3.31 Ga, 2.96–2.86 2.72–2.59 2.56–2.47 2.45–2.0 1.99–1.85 Ga 1.84–1.65 Ga. The geochemical features suggest that some sediments were sourced intermediate felsic magmatic rocks. groups detrital roughly...