Paleomagnetic data from the New England Orogen (eastern Australia) and implications for oroclinal bending

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Paleomagnetic data from the New England Orogen (eastern Australia) and implications for oroclinal bending

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作者：Uri Shaanan^a ; ^{u.shaanan@uq.edu.au" class="auth_mail" title="E-mail the corresponding author} ; Gideon Rosenbaum^a ; Sergei Pisarevsky^b ; ^c ; Fabio Speranza^d
关键词：Oroclinal bending ; Subduction rollback ; Back-arc extension ; New England Orogen ; Paleomagnetism
刊名：Tectonophysics
出版年：2015
出版时间：28 November 2015
年：2015
卷：664
期：Complete
页码：182-190
全文大小：3461 K

文摘

•: A Permian paleopole from the southernmost New England oroclines was obtained.
•: Data show no rotations relative to cratonic Australia/Gondwana after ~ 272 Ma.
•: Oroclinal bending occurred before 272 Ma and prior to the Hunter–Bowen Orogeny.
•: The New England oroclines formed in extensional setting likely by trench retreat.

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