Detrital zircon fingerprints link western North China Craton with East Gondwana during Ordovician
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- 作者：Zhentao Wanga ; gibson_wong@foxmail.com" class="auth_mail" title="E-mail the corresponding author ; wangz@cags.ac.cn" class="auth_mail" title="E-mail the corresponding author ; Hongrui Zhoub ; Xunlian Wangb ; Mianping Zhenga ; M. Santoshb ; c ; Xiuchun Jingb ; Jin Zhangd ; Yongsheng Zhanga
- 关键词：Detrital zircon geochronology ; Provenance ; North China Craton ; Gondwana ; Ordovician
- 刊名：Gondwana Research
- 出版年：2016
- 出版时间：December 2016
- 年：2016
- 卷：40
- 期：Complete
- 页码：58-76
- 全文大小：21701 K
文摘
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Linking western North China Craton with the East Gondwana in Late Ordovician.
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The Middle Ordovician detritus derived from the basement of NCC.
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The Upper Ordovician sediments sourced from the eastern Gondwana.
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A prominent tectonic shift on the western margin of the NCC at ca. 458 Ma
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A foreland basin between the western NCC and eastern Gondwana at ca. 458 Ma.