Skarn formation and trace elements in garnet and associated minerals from Zhibula copper deposit, Gangdese Belt, southern Tibet
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- 作者：Jing Xua ; b ; jing.xu01@adelaide.edu.au" class="auth_mail" title="E-mail the corresponding author ; xujing3800@126.com" class="auth_mail" title="E-mail the corresponding author ; Cristiana L. Ciobanub ; Nigel J. Cookb ; Youye Zhenga ; c ; zhyouye@163.com" class="auth_mail" title="E-mail the corresponding author ; Xiang Sunc ; Benjamin P. Waded
- 关键词：Zhibula ; Gangdese belt ; Southern Tibet ; Garnet ; Trace element substitution
- 刊名：Lithos
- 出版年：2016
- 出版时间：1 October 2016
- 年：2016
- 卷：262
- 期：Complete
- 页码：213-231
- 全文大小：6262 K
文摘
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REY fractionation trends in garnet reflect prograde-to-retrograde evolution.
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Garnet chemistry is also controlled by local environment and major oxide content.
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Garnet compositions support common fluids for skarn and nearby Cu–Mo porphyry system.
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Mo, W and Sn in skarn garnet carry implications for mineral exploration.