Garnet secondary ion mass spectrometry oxygen isotopes reveal crucial roles of pulsed magmatic fluid and its mixing with meteoric water in lode gold genesis

Lode gold deposits, which are currently the world’s major gold supply, have been shown to be generated mostly by phase separation of metamorphic fluids and/or interaction between these fluids and wall rocks. Here we use garnet oxygen isotopes by secondary ion mass spectrometry to document the crucia...

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Detalles Bibliográficos
Autores principales: Fan, Gao-Hua, Li, Jian-Wei, Valley, John W., Scicchitano, Maria Rosa, Brown, Philip E., Yang, Jin-Hui, Robinson, Paul T., Deng, Xiao-Dong, Wu, Ya-Fei, Li, Zhan-Ke, Gao, Wen-Sheng, Li, Si-Yuan, Zhao, Shao-Rui
Formato: Online Artículo Texto
Lenguaje:English
Publicado: National Academy of Sciences 2022
Materias:
Physical Sciences
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9171613/
https://www.ncbi.nlm.nih.gov/pubmed/35500124
http://dx.doi.org/10.1073/pnas.2116380119

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9171613/
https://www.ncbi.nlm.nih.gov/pubmed/35500124
http://dx.doi.org/10.1073/pnas.2116380119

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