A5087759699- Geological and Geochemical Analysis
- Geochemistry and Geologic Mapping
- Geochemistry and Geochronology of Asian Mineral Deposits
- Mineralogy and Gemology Studies
- Metal Extraction and Bioleaching
- Geochemistry and Elemental Analysis
- High-pressure geophysics and materials
- earthquake and tectonic studies
China University of Geosciences (Beijing)
2013-2024
Abstract The Y angla copper deposit ( C u reserves: 1.2 M t) in the J inshajiang– L ancangjiang– N ujiang region hina is spatially associated with inong granitoid. Zircon U – P b dating shows granitoid formed at 234.1 ± to 235.6 a, and KT 2 ore body of yields a molybdenite R e– O s model age 230.9 3.2 a. ages mineralization crystallization are identical within measurement uncertainties, suggesting genitically related I ndosinian
<p>Table S1: Results of zircon LA-ICP-MS U-Pb analyses the granite porphyry in Zhalageamu copper deposit. Table S2: Re-Os isotope molybdenite S3: arsenopyrite S4: chalcopyrite and pyrite S5: Ages Re contents different deposits southern part Great Xing’an Range.</p>
Discovered within the North Himalayan Metallogenic Belt (NHMB), Zhaxikang Pb–Zn–Ag–Sb deposit stands as sole super-large scale ore in region. This holds significant quantities of Pb and Zn (2.066 million tons at 6.38% average grade), Ag (2661 an 101.64 g/t), Sb (0.235 1.14% making it one China’s foremost Sb–polymetallic deposits. Stibnite represents main carrier this has been great attention since its initial discovery. However, trace element composition stibnite not yet determined. study...
<p>Table S1: Results of zircon LA-ICP-MS U-Pb analyses the granite porphyry in Zhalageamu copper deposit. Table S2: Re-Os isotope molybdenite S3: arsenopyrite S4: chalcopyrite and pyrite S5: Ages Re contents different deposits southern part Great Xing’an Range.</p>