Carboniferous-Permian tectonic framework and its later modifications to the area from eastern Kazakhstan to southern Altai: Insights from the Zaysan-Jimunai Basin evolution
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- 作者：Di Lia ; xdlidi@163.com" class="auth_mail" title="E-mail the corresponding author ; Dengfa Hea ; hedengfa282@263.net" class="auth_mail" title="E-mail the corresponding author ; Delong Maa ; Yong Tangb ; Yuhua Kongb ; Jieyun Tanga
- 关键词：Late Carboniferous basalts ; Carboniferous&ndash ; Permian tectonic framework ; Later modification ; Zaysan&ndash ; Jimunai Basin evolution ; Eastern Kazakhstan to southern Altai
- 刊名：Journal of Asian Earth Sciences
- 出版年：2015
- 出版时间：1 December 2015
- 年：2015
- 卷：113
- 期：part_P1
- 页码：16-35
- 全文大小：8463 K
文摘
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The ca. 313 Ma basalts from Well JC1 are defined in the Zaysan–Jimunai Basin.
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The Upper Carboniferous series formed in an island arc setting.
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Double subduction of Irtysh–Zaysan Ocean persisted until the Late Carboniferous.
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The area from eastern Kazakhstan to southern Altai experienced episodic modifications since Permian.
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