A5063383179- Geological and Geochemical Analysis
- Geochemistry and Geologic Mapping
- earthquake and tectonic studies
- High-pressure geophysics and materials
- Geochemistry and Geochronology of Asian Mineral Deposits
- Mineralogy and Gemology Studies
- Geological and Geophysical Studies
- Geochemistry and Elemental Analysis
Chinese Academy of Geological Sciences
2016-2021
Ministry of Natural Resources
2018-2021
Czech Academy of Sciences, Institute of Geology
2017
China University of Geosciences (Beijing)
2016
Xinjiang University
2011-2013
Qie Qinab, He Huangbc, Tao Wangbc*, Ruiqing Guod, Zhaochong Zhanga & Ying Tongba State Key Laboratory of Geological Processes and Mineral Resources, China University Geosciences, Beijing, Chinab Institute Geology, Chinese Academy Sciences, Chinac 3D Geology Research Centre, Survey, Chinad College Mining Engineering, Xinjiang University, Urumqi,
In this article, we report whole-rock and mineral Sm–Nd isotopic elemental Sr–Nd data of Xingdi No. 1 mafic–ultramafic intrusion in the western Kuluketage block, north-eastern Tarim. is largest belt, with an exposed area ca. 20 km2. It intruded into Palaeoproterozoic basement. Gabbro major rock type there minor olivine pyroxenite. geochronometry gabbro gives isochron age 761.2 ± 31.2 million years, identical to intrusive 2 pluton (760 6 years). The systematically enriched large ion...
Carboniferous magmatism is one of the most important tectonothermal events in Central Asian Orogenic Belt (CAOB). However, final closure time Kalamaili Ocean between East Junggar and Harlik Mountain still debated. Early (332 Ma) late (307–298 granitic from fault zone have been recognized by LA‐ICP‐MS zircon U‐Pb dating. They are both metaluminous highly fractionated I‐type belong to high‐K calc‐alkaline. The granitoids for early ε Hf ( t ) values –5.1 +8.5 with model ages (T DM2 1.78–0.83Ga,...
The origination and differentiation of rare metalbearing, alkaline granites has attracted extensive interests because their economic significance.
The Ku’erchu granitic pluton (283±4 Ma) was exposed in the eastern part of South Tianshan Orogenic Belt. granites from intrusion are mainly composed orthoclase (~45 vol. %), plagioclase (~15 quartz (~20 muscovite (~10 %) and biotite (~5 with accessory minerals including garnet, zircon Fe-Ti oxide.