Partial melting of an ancient sub-continental lithospheric mantle in the early Paleozoic intracontinental regime and its contribution to petrogenesis of the coeval peraluminous granites in South China
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- 作者：Yufang Zhonga ; b ; zhongyufang@cug.edu.cn" class="auth_mail" title="E-mail the corresponding author ; 1074292912@qq.com" class="auth_mail" title="E-mail the corresponding author ; Lianxun Wanga ; b ; Junhong Zhaoa ; b ; Lei Liuc ; Changqian Maa ; b ; Jianping Zhenga ; b ; Zejun Zhanga ; Biji Luoa ; b
- 关键词：Sub-continental lithospheric mantle ; Intracontinental orogen ; Paleozoic ; South China ; Appinite&ndash ; granite association ; Peraluminous granites
- 刊名：Lithos
- 出版年：2016
- 出版时间：1 November 2016
- 年：2016
- 卷：264
- 期：Complete
- 页码：224-238
- 全文大小：3462 K
文摘
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The appinite–granite association was formed from 444 ± 3 Ma to 452 ± 4 Ma.
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The appinites likely originated from an ancient metasomatised mantle.
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The magmatic processes include AFC, magma mingling and/or mixing.
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The appinite–granite association was formed in an intracontinental regime.
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The ancient enriched mantle has a significant contribution to some of the Paleozoic granitoids in South China.