Age and compositions of garnet in a magnesian skarn Au-Cu deposit, Tibet, implications for ore-fluid evolution

Nan Chao,Xin Chen, Jianhui Wu, Xiaoyi Wang, Yibing Lin,Decai Lin,Jianbing Li, Ye Gu,Miao Li, Junleng Lu,Hao Lin,Youye Zheng

Ore Geology Reviews(2023)

引用 0|浏览9
暂无评分
摘要
•The age of garnets (90–89 Ma) matched the age of Au-Cu mineralization (88.6 ± 0.6 Ma);•The Galale deposit is a typical Mg-skarn Au-Cu deposit;•The REE content of garnets was influenced by metasomatism and ore-forming fluids;•The high fO2 of fluids in early stages is vital for Au-Cu enrichment.
更多
查看译文
关键词
Garnet,In situ U–Pb dating,Oxygen fugacity,Mg-skarn,Metasomatism,Galale
AI 理解论文
溯源树
样例
生成溯源树,研究论文发展脉络
Chat Paper
正在生成论文摘要