首页|期刊导航|Acta Geologica Sinica(English Edition)|Oxygen Fugacity Differences Between the Tungsten-and Tin-Bearing Magmas During Reduced Magmatic Fractionation:Evidence From Apatite in Guidong and Dayishan Plutons in South China
Oxygen Fugacity Differences Between the Tungsten-and Tin-Bearing Magmas During Reduced Magmatic Fractionation:Evidence From Apatite in Guidong and Dayishan Plutons in South China
Qianqian Zhao Chunli Guo Bin Hu Binwu Zhang Jianqi Xu Ke Huang
Acta Geologica Sinica(English Edition)2026,Vol.100Issue(4):P.1126-1144,19.
Acta Geologica Sinica(English Edition)2026,Vol.100Issue(4):P.1126-1144,19.DOI:10.1111/1755-6724.70074
Oxygen Fugacity Differences Between the Tungsten-and Tin-Bearing Magmas During Reduced Magmatic Fractionation:Evidence From Apatite in Guidong and Dayishan Plutons in South China
摘要
关键词
apatite/magmatic fractionation/oxygen fugacityl tin mineralization ltungsten mineralization分类
天文与地球科学引用本文复制引用
Qianqian Zhao,Chunli Guo,Bin Hu,Binwu Zhang,Jianqi Xu,Ke Huang..Oxygen Fugacity Differences Between the Tungsten-and Tin-Bearing Magmas During Reduced Magmatic Fractionation:Evidence From Apatite in Guidong and Dayishan Plutons in South China[J].Acta Geologica Sinica(English Edition),2026,100(4):P.1126-1144,19.基金项目
supported bythe Deep Earth probe and Mineral Resources Exploration-National Science and Technology Major Project(2025ZD1009001) (2025ZD1009001)
the National Natural Science Foundation of China(92162210)。 (92162210)