The 1320 Ma intracontinental Wongawobbin Basin, Pilbara, Western Australia: A far-field response to Albany-Fraser-Musgrave tectonics
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- 作者：Stephen Sheppard ; stephen.sheppard@curtin.edu.au" class="auth_mail" title="E-mail the corresponding author ; Bryan Krapež bryan.krapez@bigpond.com" class="auth_mail" title="E-mail the corresponding author ; Jian-Wei Zi j.zi@curtin.edu.au" class="auth_mail" title="E-mail the corresponding author ; Birger Rasmussen B.Rasmussen@curtin.edu.au" class="auth_mail" title="E-mail the corresponding author ; Ian Fletcher ianfletcher47@bigpond.com" class="auth_mail" title="E-mail the corresponding author
- 关键词：Zircon ; SHRIMP geochronology ; Mesoproterozoic ; Pilbara Craton ; Eel Creek Formation
- 刊名：Precambrian Research
- 出版年：2016
- 出版时间：October 2016
- 年：2016
- 卷：285
- 期：Complete
- 页码：58-79
- 全文大小：2486 K
文摘
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Formerly undated sedimentary succession on the edge of the Pilbara Craton.
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Zircon geochronology of tuffs constrains deposition of succession to c. 1320 Ma.
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Sedimentation is coeval with intense tectonic activity in the Albany–Fraser and Musgrave Orogens.
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Newly identified intracontinental basin was probably a far-field response to convergent margin tectonism.
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