Zircons traced from the 700-500 Ma Transgondwanan Supermountains and the Gamburtsev Subglacial Mountains to the Ordovician Lachlan Orogen, Cretaceous Ceduna Delta, and modern Channel Country, central-southern Australia
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- 作者：J.J. Veevers ; john.veevers@mq.edu.au" class="auth_mail" title="E-mail the corresponding author ; E.A. Belousova ; A. Saeed
- 关键词：U&ndash ; Pb detrital zircon age ; Hf-isotopes ; SE Australia ; Provenance ; Gamburtsev Subglacial Mountains ; East African&ndash ; Antarctic Orogen
- 刊名：Sedimentary Geology
- 出版年：2016
- 出版时间：1 April 2016
- 年：2016
- 卷：334
- 期：Complete
- 页码：115-141
- 全文大小：5277 K
文摘
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700–500 Ma zircons in eastern Australia came from the Transgondwanan Supermountains.
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~100 Ma zircons came from the magmatic arc and LIP alongside East Gondwanaland.
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Both were shed west from the ≤100 Ma uplifted E Australia to fill the Ceduna Delta.