Petrogenesis and tectonic significance of the late Triassic mafic dikes and felsic volcanic rocks in the East Kunlun Orogenic Belt, Northern Tibet Plateau
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- 作者：Yan Hua ; roba.hu@foxmail.com" class="auth_mail" title="E-mail the corresponding author ; Yaoling Niua ; b ; c ; yaoling.niu@foxmail.com" class="auth_mail" title="E-mail the corresponding author ; Jiyong Lia ; Lei Yed ; Juanjuan Konga ; Shuo Chena ; Yu Zhangd ; Guorui Zhangd
- 关键词：Alkaline mafic dikes ; Felsic volcanic rocks ; Subcontinental lithospheric mantle ; Crustal anatexis ; Post-collision ; East Kunlun Orogenic Belt
- 刊名：Lithos
- 出版年：2016
- 出版时间：15 February 2016
- 年：2016
- 卷：245
- 期：Complete
- 页码：205-222
- 全文大小：2741 K
文摘
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The (sub-)volcanic rocks from the East Kunlun Orogenic Belt formed at late Triassic.
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Mafic dikes are derived from the metasomatized subcontinental lithospheric mantle.
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Felsic volcanic rocks evolved from melts of juvenile crustal materials.
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The (sub-)volcanic rocks are associated with post-collisional extension.