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• W2065651411 abstract "Research Article| February 01, 2004 Structural expression of oblique seafloor spreading in the Macquarie Island ophiolite, Southern Ocean Peter A. Rivizzigno; Peter A. Rivizzigno 1Division of Earth and Ocean Sciences, Nicholas School of the Environment and Earth Sciences, Duke University, Durham, North Carolina 27708, USA Search for other works by this author on: GSW Google Scholar Jeffrey A. Karson Jeffrey A. Karson 1Division of Earth and Ocean Sciences, Nicholas School of the Environment and Earth Sciences, Duke University, Durham, North Carolina 27708, USA Search for other works by this author on: GSW Google Scholar Author and Article Information Peter A. Rivizzigno 1Division of Earth and Ocean Sciences, Nicholas School of the Environment and Earth Sciences, Duke University, Durham, North Carolina 27708, USA Jeffrey A. Karson 1Division of Earth and Ocean Sciences, Nicholas School of the Environment and Earth Sciences, Duke University, Durham, North Carolina 27708, USA Publisher: Geological Society of America Received: 24 Jun 2003 Revision Received: 24 Oct 2003 Accepted: 29 Oct 2003 First Online: 03 Mar 2017 Online ISSN: 1943-2682 Print ISSN: 0091-7613 Geological Society of America Geology (2004) 32 (2): 125–128. https://doi.org/10.1130/G19906.1 Article history Received: 24 Jun 2003 Revision Received: 24 Oct 2003 Accepted: 29 Oct 2003 First Online: 03 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation Peter A. Rivizzigno, Jeffrey A. Karson; Structural expression of oblique seafloor spreading in the Macquarie Island ophiolite, Southern Ocean. Geology 2004;; 32 (2): 125–128. doi: https://doi.org/10.1130/G19906.1 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 The Macquarie Island ophiolite is an uplifted block of oceanic crust formed at the Australia-Pacific spreading center between 12 and 9 Ma. The sense of motion and geological processes across this plate boundary reflect an evolution from orthogonal spreading through progressively more oblique spreading to the present-day transpressional regime. The crust that makes up the island was formed during an interval of oblique spreading along east-trending spreading segments punctuated by a series of northwest-trending discontinuities. The discontinuities are accommodation zones marked by oblique-slip dextral-normal faults, localized dikes and lava flows, and extensive hydrothermal alteration, indicating that these zones were active near the spreading axis. These features provide a window into the internal structure of oceanic crust generated by oblique spreading. 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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• W2065651411 title "Structural expression of oblique seafloor spreading in the Macquarie Island ophiolite, Southern Ocean" @default.
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