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- W1999528031 abstract "Research Article| March 01, 2001 Cretaceous demise of the Moa plate and strike-slip motion at the Gondwana margin Rupert Sutherland; Rupert Sutherland 1Institute of Geological & Nuclear Sciences, P.O. Box 30-368, Lower Hutt, New Zealand Search for other works by this author on: GSW Google Scholar Chris Hollis Chris Hollis 1Institute of Geological & Nuclear Sciences, P.O. Box 30-368, Lower Hutt, New Zealand Search for other works by this author on: GSW Google Scholar Author and Article Information Rupert Sutherland 1Institute of Geological & Nuclear Sciences, P.O. Box 30-368, Lower Hutt, New Zealand Chris Hollis 1Institute of Geological & Nuclear Sciences, P.O. Box 30-368, Lower Hutt, New Zealand Publisher: Geological Society of America Received: 06 Jul 2000 Revision Received: 27 Nov 2000 Accepted: 01 Dec 2000 First Online: 02 Jun 2017 Online ISSN: 1943-2682 Print ISSN: 0091-7613 Geological Society of America Geology (2001) 29 (3): 279–282. https://doi.org/10.1130/0091-7613(2001)029<0279:CDOTMP>2.0.CO;2 Article history Received: 06 Jul 2000 Revision Received: 27 Nov 2000 Accepted: 01 Dec 2000 First Online: 02 Jun 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation Rupert Sutherland, Chris Hollis; Cretaceous demise of the Moa plate and strike-slip motion at the Gondwana margin. Geology 2001;; 29 (3): 279–282. doi: https://doi.org/10.1130/0091-7613(2001)029<0279:CDOTMP>2.0.CO;2 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyGeology Search Advanced Search Abstract Radiolaria and paleomagnetic data from Deep Sea Drilling Project Sites 595 and 596 indicate that Early Cretaceous seafloor was formed at moderate to high latitudes in the Pacific. This inference requires a Cretaceous spreading ridge south of the Pacific-Phoenix Ridge and substantial dextral strike-slip motion at the Gondwana margin. The previously unrecognized southern oceanic plate, called here the Moa plate, was obliquely subducted beneath the Gondwana margin, and material accreted from it is now part of the Eastern province of New Zealand. You do not have access to this content, please speak to your institutional administrator if you feel you should have access." @default.
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- W1999528031 title "Cretaceous demise of the Moa plate and strike-slip motion at the Gondwana margin" @default.
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