A5067142424- Geological and Geochemical Analysis
- High-pressure geophysics and materials
- Geochemistry and Geologic Mapping
- earthquake and tectonic studies
- Geochemistry and Elemental Analysis
- Geology and Paleoclimatology Research
- Geochemistry and Geochronology of Asian Mineral Deposits
- Geological and Geophysical Studies
- Radioactive element chemistry and processing
- X-ray Diffraction in Crystallography
- Crystallization and Solubility Studies
- Hydrocarbon exploration and reservoir analysis
- Isotope Analysis in Ecology
- Mineralogy and Gemology Studies
- Advanced Photocatalysis Techniques
- Paleontology and Stratigraphy of Fossils
- Extraction and Separation Processes
- Consumer Perception and Purchasing Behavior
- Microbial Fuel Cells and Bioremediation
- Geological Studies and Exploration
- Adsorption and biosorption for pollutant removal
- Methane Hydrates and Related Phenomena
- Analytical chemistry methods development
- Wastewater Treatment and Nitrogen Removal
- Electrocatalysts for Energy Conversion
Chinese Academy of Sciences
2016-2025
Institute of Geology and Geophysics
2016-2025
University of Chinese Academy of Sciences
2013-2025
Zhengzhou University of Light Industry
2025
Changchun University of Science and Technology
2024
Dalian University of Technology
2014-2024
Guangzhou University
2024
China University of Mining and Technology
2024
China National Petroleum Corporation (China)
2023-2024
Xinjiang University
2024
Since the 1970s, splitting water using solar energy has been a focus of great attention as possible means for converting to chemical in form clean and renewable hydrogen fuel. Approaches include photocatalytic with homogeneous or heterogeneous photocatalysts, photoelectrochemical photoelectrocatalytic (PEC) PEC cell, electrolysis photovoltaic cells coupled electrocatalysts. Though many materials are capable photocatalytically producing and/or oxygen, overall conversion efficiency is still...
The North China Craton (NCC) was originally formed by the amalgamation of eastern and western blocks along an orogenic belt at ∼1.9 Ga. After cratonization, NCC essentially stable until Mesozoic, when intense felsic magmatism related mineralization, deformation, pull-apart basins, exhumation deep crust widely occurred, indicative destruction or decratonization. Accompanying this significant removal cratonic keel lithospheric transformation, whereby thick (∼200 km) refractory Archean...
Abstract The tectonic setting of the Eastern Asian continental margin in Jurassic is highly controversial. In current study, we have selected Heilongjiang complex located at western Jiamusi Massif northeastern China for geochronological investigation to address this issue. Field and petrographic investigations indicate that composed predominately granitic gneiss, marble, mafic‐ultramafic rocks, blueschist, greenschist, quartzite, muscovite‐albite schist two‐mica were tectonically...
Baddeleyite has long been recognized as one of the most important U-bearing minerals for dating silica undersaturated igneous rocks. Age determination baddeleyite calls analysis within small volumes using high-resolution secondary ion mass spectrometry (SIMS) because its minuscule grain size well potential altered domains or micro-inclusions. However, precise SIMS U–Pb hampered owing to crystal orientation effects that bias Pb/U ratio measured in baddeleyite. In this study we carried out a...
Research Article| June 01, 2008 Mesozoic decratonization of the North China block Jin-Hui Yang; Yang * 1State Key Laboratory Lithospheric Evolution, Institute Geology and Geophysics, Chinese Academy Sciences, P.O. Box 9825, Beijing 100029, *E-mail: jinhui@mail.igcas.ac.cn. Search for other works by this author on: GSW Google Scholar Fu-Yuan Wu; Wu Simon A. Wilde; Wilde 2Department Applied Geology, Curtin University Technology, U1987, Perth, Western Australia 6845, Elena Belousova; Belousova...