Zircon U-Pb ages and Sr-Nd-Hf isotopes of the highly fractionated granite with tetrad REE patterns in the Shamai tungsten deposit in eastern Inner Mongolia, China: Implications for the timing of mineralization and ore genesis
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- 作者：Si-Hong Jianga ; jiangsihong1@163.com" class="auth_mail" title="E-mail the corresponding author ; Leon Bagasa ; b ; Peng Huc ; Ning Hana ; Chun-Liang Chena ; Yuan Liua ; Huan Kanga
- 关键词：Geochronology ; REE tetrad effect ; Sr&ndash ; Nd&ndash ; Hf isotopes ; Tungsten deposit ; Shamai ; China
- 刊名：Lithos
- 出版年：2016
- 出版时间：15 September 2016
- 年：2016
- 卷：261
- 期：Complete
- 页码：322-339
- 全文大小：2396 K
文摘
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Shamai Granite associated with W mineralization is a highly fractionated peraluminous granite with tetrad REE patterns.
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The W mineralization is related to the prolonged magmatic–hydrothermal history.
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The Shamai Granite was formed in an extensional setting.