Fluid Inclusion and Stable Isotope Geochemistry of the Shangxu Gold Deposit, Northern Tibet

Fluid Inclusion and Stable Isotope Geochemistry of the Shangxu Gold Deposit, Northern Tibet

Objective The Shangxu gold deposit is located in the south of the middle Bangong-Nujiang suture zone in northern Tibet. The origin of this deposit as an orogenic gold deposit is debatable. The study of the Shangxu deposit has a profound implication on gold exploration in the Bangong- Nujiang metallo...

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Veröffentlicht in:Acta geologica Sinica (Beijing) 2016-08, Vol.90 (4), p.1545-1546
Hauptverfasser: Yingru, PEI, Zhusen, YANG, Xiaoyan, ZHAO, Xiong, ZHANG, Wang, MA, Jingtao, MAO
Format: Artikel
Sprache:eng
Schlagworte:
成矿带
流体包裹体
班公湖-怒江缝合带
矿床
稳定同位素地球化学
西藏北部
西藏南部
金矿
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Zusammenfassung:Objective The Shangxu gold deposit is located in the south of the middle Bangong-Nujiang suture zone in northern Tibet. The origin of this deposit as an orogenic gold deposit is debatable. The study of the Shangxu deposit has a profound implication on gold exploration in the Bangong- Nujiang metallogenic belt and can also improve our understanding of gold mineralization in northern Tibet.
ISSN:1000-9515
1755-6724
DOI:10.1111/1755-6724.12789