A5004123281- Geological and Geochemical Analysis
- Geochemistry and Geologic Mapping
- Geochemistry and Geochronology of Asian Mineral Deposits
- earthquake and tectonic studies
- High-pressure geophysics and materials
- Hydrocarbon exploration and reservoir analysis
- Pneumocystis jirovecii pneumonia detection and treatment
- Hydraulic and Pneumatic Systems
- Infectious Diseases and Tuberculosis
- Fluid Dynamics and Turbulent Flows
- Smart Grid and Power Systems
- Geochemistry and Elemental Analysis
- Tuberculosis Research and Epidemiology
- Plasma and Flow Control in Aerodynamics
- Power Systems and Technologies
- Power Systems and Renewable Energy
China University of Geosciences (Beijing)
2021-2024
Sichuan University
2024
Northwestern Polytechnical University
2024
National Taiwan University
2016
Abstract Crustal growth is commonly associated with porphyry deposit formation whether in continental arcs or collisional orogens. The Miocene high-K calc-alkaline granitoids the Gangdese belt southern Tibet, copper deposits, are derived from juvenile lower crust input lithospheric mantle trachytic magmas, and characterized by adakitic affinity high-Sr/Y La/Yb ratios as well high Mg# more evolved isotopic ratios. Researchers have argued, metal fertilization was mainly formed previous...
The post-collisional Gangdese metallogenic belt with over 45 Mt Cu has attracted worldwide attention. We report the whole-rock geochemistry, zircon SIMS U–Pb geochronology, and in situ Hf–O isotopic compositions of Jiama deposit belt. intermediate to felsic intrusive rocks are characterized by high SiO2 (64.8 78.8 wt. %) Al2O3 (12.1 16.3 contents, Sr/Y ratios (43–74), showing geochemical characteristics adakites. Zircons from four intrusives yield ages 16.19 ± 0.20 Ma, 15.67 0.32 15.44 0.16...
Slab tearing is widely reported in oceanic slabs; however, continental slabs still not very well understood. Geophysical data have shown the existence of Indian lithosphere underneath Yadong-Gulu rift southern Tibet. Along this rift, Jiacun lamprophyres and Yangying trachytes comprise youngest alkaline volcanic rocks Himalayan-Tibetan orogen, hence provide evidence for understanding operation slab tearing. lamprophyres, with an age 13 Ma as determined by Ar-Ar dating, are only outcrop...
Abstract Porphyry Cu deposits (PCDs) in collisional orogens are new targets for modern mineral exploration. A series of post-collisional (Miocene; 22-12Ma) porphyry copper deposit with reserve over 45 Mt have been discovered the Gangdese magmatic belt, southern Tibet. These magmas derived from partial melting sulfide-bearing Tibetan juvenile lower crust fertile many aspects, such as high oxidation state, and rich volatiles water, S, Cl, but some individual plutons ended up economic...
Two supplemental pictures and five tables. The exhibit the Nd-Hf isotopic spatial distribution of Gangdese belt magmatic rocks, southern Tibet, by using average values per 0.5 longitude (Fig. S1) two additional magma mixing models related to Jurassic Cretaceous Tibet S2). talbes contain all data used in this research their references.
Two supplemental pictures and five tables. The exhibit the Nd-Hf isotopic spatial distribution of Gangdese belt magmatic rocks, southern Tibet, by using average values per 0.5 longitude (Fig. S1) two additional magma mixing models related to Jurassic Cretaceous Tibet S2). talbes contain all data used in this research their references.
Two supplemental pictures and five tables. The exhibit the Nd-Hf isotopic spatial distribution of Gangdese belt magmatic rocks, southern Tibet, by using average values per 0.5 longitude (Fig. S1) two additional magma mixing models related to Jurassic Cretaceous Tibet S2). talbes contain all data used in this research their references.
Two supplemental pictures and five tables. The exhibit the Nd-Hf isotopic spatial distribution of Gangdese belt magmatic rocks, southern Tibet, by using average values per 0.5 longitude (Fig. S1) two additional magma mixing models related to Jurassic Cretaceous Tibet S2). talbes contain all data used in this research their references.
Two supplemental pictures and five tables. The exhibit the Nd-Hf isotopic spatial distribution of Gangdese belt magmatic rocks, southern Tibet, by using average values per 0.5 longitude (Fig. S1) two additional magma mixing models related to Jurassic Cretaceous Tibet S2). talbes contain all data used in this research their references.
Two supplemental pictures and five tables. The exhibit the Nd-Hf isotopic spatial distribution of Gangdese belt magmatic rocks, southern Tibet, by using average values per 0.5 longitude (Fig. S1) two additional magma mixing models related to Jurassic Cretaceous Tibet S2). talbes contain all data used in this research their references.
Two supplemental pictures and five tables. The exhibit the Nd-Hf isotopic spatial distribution of Gangdese belt magmatic rocks, southern Tibet, by using average values per 0.5 longitude (Fig. S1) two additional magma mixing models related to Jurassic Cretaceous Tibet S2). talbes contain all data used in this research their references.
Two supplemental pictures and five tables. The exhibit the Nd-Hf isotopic spatial distribution of Gangdese belt magmatic rocks, southern Tibet, by using average values per 0.5 longitude (Fig. S1) two additional magma mixing models related to Jurassic Cretaceous Tibet S2). talbes contain all data used in this research their references.