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• W2321479880 abstract "Research Article| November 01, 2011 Inverted metamorphic sequences in Alpine fault mylonites produced by oblique shear within a plate boundary fault zone, New Zealand Alan F. Cooper; Alan F. Cooper Geology Department, University of Otago, Dunedin 9054, New Zealand Search for other works by this author on: GSW Google Scholar Richard J. Norris Richard J. Norris Geology Department, University of Otago, Dunedin 9054, New Zealand Search for other works by this author on: GSW Google Scholar Geology (2011) 39 (11): 1023–1026. https://doi.org/10.1130/G32273.1 Article history received: 22 Mar 2011 rev-recd: 15 Jun 2011 accepted: 15 Jun 2011 first online: 09 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 Alan F. Cooper, Richard J. Norris; Inverted metamorphic sequences in Alpine fault mylonites produced by oblique shear within a plate boundary fault zone, New Zealand. Geology 2011;; 39 (11): 1023–1026. doi: https://doi.org/10.1130/G32273.1 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 Low-grade albite- and peristerite-mylonites occur as a northeast-tapering, 200–300 m wide zone structurally above basal cataclasite on the Alpine fault (New Zealand). They form an inverted metamorphic sequence grading eastward into an ∼1-km-wide, amphibolite-facies−derived mylonite zone in the hanging wall. Their mineralogy matches low-grade protoliths that occur 100–110 km to the southeast. This displacement is compatible with distributed lateral and vertical shear within the mylonite zone since inception of significant convergence on the plate boundary in the late Neogene. 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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• W2321479880 title "Inverted metamorphic sequences in Alpine fault mylonites produced by oblique shear within a plate boundary fault zone, New Zealand" @default.
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