The timing of final closure along the Changchun-Yanji suture zone: Constraints from detrital zircon U-Pb dating of the Triassic Dajianggang Formation, NE China
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- 作者：Bin Wanga ; wangbinjlu@qq.com" class="auth_mail" title="E-mail the corresponding author ; Jian-Bo Zhoua ; zhoujianbo@jlu.edu.cn" class="auth_mail" title="E-mail the corresponding author ; Simon A. Wildea ; b ; s.wilde@curtin.edu.au" class="auth_mail" title="E-mail the corresponding author ; Xing-Zhou Zhanga ; xzzhang@jlu.edu.cn" class="auth_mail" title="E-mail the corresponding author ; Shou-Mai Renc ; realshaw@vip.sina.com" class="auth_mail" title="E-mail the corresponding author
- 关键词：Changchun&ndash ; Yanji suture ; Dajianggang Formation ; U&ndash ; Pb dating ; Late Triassic ; Jilin&ndash ; Heilongjiang high-pressure belt ; Paleo-Pacific Ocean
- 刊名：Lithos
- 出版年：2016
- 出版时间：15 September 2016
- 年：2016
- 卷：261
- 期：Complete
- 页码：216-231
- 全文大小：3370 K
文摘
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Dajianggang Formation yields young peak age of 225 Ma. Final closure timing of the CY suture was in the Late Triassic.
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The timing of final closure along the suture was in the Late Triassic.
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The Late Triassic marked the switch in subduction from the Paleo-Asian Ocean to the Paleo-Pacific Ocean.