Eocene slab breakoff of Neotethys as suggested by dioritic dykes in the Gangdese magmatic belt, southern Tibet
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- 作者：Xuxuan Maa ; xuxuan.ma@hotmail.com" class="auth_mail" title="E-mail the corresponding author ; Zhiqin Xua ; Joseph G. Meertb
- 关键词：Eocene ; Dioritic dyke ; Slab breakoff ; Gangdese ; Tibet
- 刊名：Lithos
- 出版年：2016
- 出版时间：April 2016
- 年：2016
- 卷：248-251
- 期：Complete
- 页码：55-65
- 全文大小：3480 K
文摘
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The dioritic dykes were dated to be emplaced at ca. 41 Ma.
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The magma source of the dykes is mainly dominated by lithospheric mantle.
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The slab breakoff played a key role in the formation of the dykes.