supported by grants from the National Natural Science Foundation of China(42073044);National Key R&D Program of China(2023YFC2906801);Geological Exploration Fund of Guizhou Province(No.2024-2;520000214TLCOG7DGTNRG);Youth Innovation Promotion Association,Chinese Academy of Sciences(2022402);Science and Technology Foundation of Guizhou Province(Qiankehepingtairencai-CXTD[2021]007);West Light Foundation of the Chinese Academy of Sciences(xbzg-zdsys-202108).
The gold-bearing arsenian pyrite in Carlin-type gold deposits typically grows around the gold/arsenic-poor pyrite core,forming core-rim textured pyrite.However,the causes of rim pyrite precipitation around the early-f...
supported financially by project 2014CB440905 under the Major State Basic Research Development Program of China (973 Program);the 12th Five-Year Plan Project of State Key Laboratory of Ore-deposit Geochemistry, Chinese Academy of Sciences (SKLODG-ZY125-01)
The Shuiyindong gold deposit is one of the most famous and largest Carlin-type gold deposits in China and is located in southwest Guizhou, in the eastern part of the Huijiabao anticline. The Shuiyindong's gold mineral...
supported jointly by the State Science and Technology Supporting Program (2006BAB01A13);the self-research project funded by the State Key Laboratory of Ore Deposit Geochemistry (Ore Deposit Special Research Project 2008.3-2);Guizhou Provincial Bureau of Geology and Mineral Resource Exploration and Development [Qian Di Kuang Ke (2009) No. 11]
The Shuiyindong deposit is one of the largest (more than 100 tonnes of Au) and highest grade (more than 7×10-6-10×10-6), strata-bound Carlintype gold deposits in southwestern Guizhou Province, China. The deposit is ...