A5056305324- Geological and Geochemical Analysis
- Geochemistry and Geologic Mapping
- Geochemistry and Elemental Analysis
- earthquake and tectonic studies
- High-pressure geophysics and materials
- Paleontology and Stratigraphy of Fossils
- Geochemistry and Geochronology of Asian Mineral Deposits
- Radioactive element chemistry and processing
- Geoscience and Mining Technology
- Geomagnetism and Paleomagnetism Studies
- Geology and Paleoclimatology Research
- Geomechanics and Mining Engineering
- Hydrocarbon exploration and reservoir analysis
- Analytical chemistry methods development
- Radioactive contamination and transfer
- Clay minerals and soil interactions
- Genetics, Aging, and Longevity in Model Organisms
- Mobile Agent-Based Network Management
- Graphene research and applications
- Chromium effects and bioremediation
- Geological and Geophysical Studies
- Metallurgy and Cultural Artifacts
- Groundwater and Isotope Geochemistry
- Chemical Synthesis and Characterization
- Extraction and Separation Processes
University of Chinese Academy of Sciences
2017-2024
Chinese Academy of Sciences
2015-2024
Institute of Geology and Geophysics
2015-2024
China University of Mining and Technology
2024
Air Force Medical University
2016-2018
Kunming University
2015
Institute of Geology and Geophysics
2013
Development Research Center
2012
China Geological Survey
2012
Sheng Jing Hospital
2001
Abstract MicroRNAs (miRNAs) interfere with the translation of specific target mRNAs and are thought to thereby regulate many cellular processes. However, role miRNAs in osteoblast mechanotransduction remains be defined. In this study, we investigated ability a miRNA respond different mechanical environments mechano-induced differentiation. First, demonstrated that miR-33-5p expressed by osteoblasts is sensitive multiple environments, microgravity fluid shear stress. We then confirmed promote...
Abstract: The Chinese Altai–East Junggar collage in the southern Altaids hosts three metallogenic belts, which are, from north to south: (1) a volcanogenic massive sulphide (VMS) Cu–Pb–Zn belt; (2) belt of shear zone-related gold deposits; (3) porphyry Cu–Au–Mo belt. VMS deposits formed two pulses ( c . 405 Ma and 375 Ma) Altai arc. developed East arc, first synchronous with mineralization, third at 330 Ma. late Carboniferous Permian contact between arcs. Time–space distributions diverse ore...
Abstract Banded iron formations (BIFs) are among the few chemical sedimentary archives that capture biogeo-chemical evolution of Fe cycling and redox early Earth. Although biologically recycled continental has been previously proposed to be a significant source in BIFs deposited from stratified ocean at onset Great Oxidation Event (GOE; ~2.5–2.2 Ga), constraining sources pathways Archean remains challenging. Here we present major trace element Fe-Nd-Cr isotope data for largest BIF (i.e.,...
The Paleoproterozoic (~2.38–2.21 Ga) Yuanjiacun banded iron formation (BIF), located in Shanxi Province, is a Superior-type BIF the North China craton. This within metasedimentary rock succession of Formation, lower Luliang Group, which has undergone greenschist-facies metamor phism. Iron oxide (magnetite and hematite), carbonate, silicate facies are all present iron-rich layers. eastward transition from carbonate- into oxide-facies formations accompanied by change mineralogical composition...
The Ashele Cu-Zn deposit is a typical VMS in Chinese Altay located the southern margin of Altaid orogen. occurred polyphase fold system, and main orebody at hinge syncline. All orebodies show lenticular form, are stratabound by suite early to middle Devonian bimodal volcanic rocks. hosting basalt low K tholeiite characterized with high Mg, Fe, Ca K, Ti. These basalts flat REE pattern Ce negative anomaly (Ce/Ce* 0.73–0.76). Niobium, Ta, Zr, Hf depleted Rb, Ba, Th, U, Sr, Pb enriched respect...