A5059267802- Geological and Geochemical Analysis
- earthquake and tectonic studies
- Geochemistry and Geologic Mapping
- High-pressure geophysics and materials
- Hydrocarbon exploration and reservoir analysis
- Geochemistry and Geochronology of Asian Mineral Deposits
- Geochemistry and Elemental Analysis
- Hydraulic Fracturing and Reservoir Analysis
- Geoscience and Mining Technology
- Geological and Geophysical Studies
- Coal Properties and Utilization
- Radioactive element chemistry and processing
- Geothermal Energy Systems and Applications
- Geological formations and processes
- Geomechanics and Mining Engineering
- Paleontology and Stratigraphy of Fossils
- Seismic Imaging and Inversion Techniques
- Reservoir Engineering and Simulation Methods
- Geology and Paleoclimatology Research
- Groundwater flow and contamination studies
- Geological Studies and Exploration
- Metallurgical Processes and Thermodynamics
- Plant Diversity and Evolution
- Clay minerals and soil interactions
- Molecular spectroscopy and chirality
Institute of Geology and Geophysics
2015-2024
Chinese Academy of Sciences
2015-2024
University of Chinese Academy of Sciences
2016-2024
Chinese Academy of Geological Sciences
1998-2024
Ministry of Natural Resources
2024
Karamay Central Hospital of Xinjiang
2021
Czech Academy of Sciences, Institute of Geology
2021
Planetary Science Institute
2019
Mineral Resources
2019
Bureau of Geology and Mineral Exploration and Development of Guizhou Province
2018
Abstract Sulfur belongs among H 2 O, CO , and Cl as one of the key volatiles in Earth’s chemical cycles. High oxygen fugacity, sulfur concentration, δ 34 S values volcanic arc rocks have been attributed to significant sulfate addition by slab fluids. However, speciation, flux, isotope composition slab-dehydrated fluids remain unclear. Here, we use high-pressure enclosed veins provide direct constraints on subduction zone recycling for a typical oceanic lithosphere. Textural thermodynamic...
The western Tianshan high‐pressure/low‐temperature orogenic belt in NW China contains eclogite‐facies metavolcanic rocks and omphacite‐bearing blueschists. Previous Sm‐Nd (omphacite, garnet, glaucophane, whole rock) 40Ar/39Ar (crossite) dating of has suggested an age ca. 345 Ma as the best approximation for timing peak metamorphic conditions. samples described here are blueschist‐facies that formed during or after transition from to epidote‐blueschist‐facies subsequently experienced...
Abstract The South Tianshan Orogen marks the final assembly of southwestern Central Asian Orogenic Belt (CAOB) and Karakum–Tarim cratons. Here we present an integrated mineralogical, geochemical, geochronological study Wuwamen ophiolitic mélange in to better understand tectonic evolution western CAOB its links Gondwana Pangea. Mantle peridotites with mineral compositions similar those abyssal basalts N‐MORB geochemical affinities suggest that ophiolite was formed a mid‐ocean ridge setting....