Matches in SemOpenAlex for { <https://semopenalex.org/work/W1973020270> ?p ?o ?g. }
- W1973020270 endingPage "1038" @default.
- W1973020270 startingPage "1025" @default.
- W1973020270 abstract "Research Article| August 01, 2001 Southeastern Lewis Hills (Bay of Islands Ophiolite): Geology of a deeply eroded, inside-corner, ridge-transform intersection Günter Suhr; Günter Suhr 1Institut für Mineralogie und Geochemie, Universität zu Köln, Zülpicher Strasse 49b, 50674 Köln, Germany, and Max-Planck- Institut für Chemie, Postfach 3060, 55020 Mainz, Germany Search for other works by this author on: GSW Google Scholar Peter A. Cawood Peter A. Cawood 2Tectonics Special Research Centre, School of Applied Geology, Curtin University, GPO Box U1987, Perth, Western Australia 6845, Australia Search for other works by this author on: GSW Google Scholar Author and Article Information Günter Suhr 1Institut für Mineralogie und Geochemie, Universität zu Köln, Zülpicher Strasse 49b, 50674 Köln, Germany, and Max-Planck- Institut für Chemie, Postfach 3060, 55020 Mainz, Germany Peter A. Cawood 2Tectonics Special Research Centre, School of Applied Geology, Curtin University, GPO Box U1987, Perth, Western Australia 6845, Australia Publisher: Geological Society of America Received: 29 Jul 1999 Revision Received: 25 Apr 2000 Accepted: 26 Sep 2000 First Online: 01 Jun 2017 Online ISSN: 1943-2674 Print ISSN: 0016-7606 Geological Society of America GSA Bulletin (2001) 113 (8): 1025–1038. https://doi.org/10.1130/0016-7606(2001)113<1025:SLHBOI>2.0.CO;2 Article history Received: 29 Jul 1999 Revision Received: 25 Apr 2000 Accepted: 26 Sep 2000 First Online: 01 Jun 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn Email Permissions Search Site Citation Günter Suhr, Peter A. Cawood; Southeastern Lewis Hills (Bay of Islands Ophiolite): Geology of a deeply eroded, inside-corner, ridge-transform intersection. GSA Bulletin 2001;; 113 (8): 1025–1038. doi: https://doi.org/10.1130/0016-7606(2001)113<1025:SLHBOI>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 SocietyGSA Bulletin Search Advanced Search Abstract The Lewis Hills massif (Bay of Islands Ophiolite, Newfoundland) preserves a deeply eroded transform fault. A major, low-angle, extensional mylonite zone is next to the transform assemblage and probably merges laterally into it. The mylonite developed in a high-temperature environment and occurs at the top of relatively rigid lithospheric mantle. The lithospheric mantle represents exhumed, older, arc-type basement of the Little Port Complex that is also exposed across the transform in the western Lewis Hills. It differs dramatically from an asthenospheric mantle unit of the Bay of Islands Complex, exposed in the eastern Lewis Hills, that formed in a spreading ridge environment.The fossil ridge-transform segment and associated low-angle normal fault in the Lewis Hills formed at an inside-corner structural setting similar to recently discovered core complexes at oceanic ridge-transform intersections. However, the Lewis Hills segment developed in a setting where a spreading center propagated across a transform margin and rifted older arc-type lithosphere. Factors that contributed to formation of the low-angle detachment fault are the lithospheric nature of the mantle basement, rheological weakening and strain focusing by intrusive sills, and weak lateral coupling realized by the extensional transform assemblage. You do not have access to this content, please speak to your institutional administrator if you feel you should have access." @default.
- W1973020270 created "2016-06-24" @default.
- W1973020270 creator A5006685240 @default.
- W1973020270 creator A5089544871 @default.
- W1973020270 date "2001-08-01" @default.
- W1973020270 modified "2023-10-17" @default.
- W1973020270 title "Southeastern Lewis Hills (Bay of Islands Ophiolite): Geology of a deeply eroded, inside-corner, ridge-transform intersection" @default.
- W1973020270 cites W1900034279 @default.
- W1973020270 cites W1968824256 @default.
- W1973020270 cites W1969731310 @default.
- W1973020270 cites W1970166457 @default.
- W1973020270 cites W1975394824 @default.
- W1973020270 cites W1978153511 @default.
- W1973020270 cites W1979888630 @default.
- W1973020270 cites W1993771392 @default.
- W1973020270 cites W1995894852 @default.
- W1973020270 cites W1997964291 @default.
- W1973020270 cites W2000846875 @default.
- W1973020270 cites W2005521268 @default.
- W1973020270 cites W2005864914 @default.
- W1973020270 cites W2006712012 @default.
- W1973020270 cites W2007711398 @default.
- W1973020270 cites W2008934623 @default.
- W1973020270 cites W2011401090 @default.
- W1973020270 cites W2012181872 @default.
- W1973020270 cites W2012556758 @default.
- W1973020270 cites W2025364748 @default.
- W1973020270 cites W2035929843 @default.
- W1973020270 cites W2043473102 @default.
- W1973020270 cites W2045859284 @default.
- W1973020270 cites W2048824368 @default.
- W1973020270 cites W2048903462 @default.
- W1973020270 cites W2050248908 @default.
- W1973020270 cites W2051469270 @default.
- W1973020270 cites W2052074832 @default.
- W1973020270 cites W2052837701 @default.
- W1973020270 cites W2056915320 @default.
- W1973020270 cites W2058589370 @default.
- W1973020270 cites W2060655431 @default.
- W1973020270 cites W2064724218 @default.
- W1973020270 cites W2069801129 @default.
- W1973020270 cites W2074213862 @default.
- W1973020270 cites W2087239287 @default.
- W1973020270 cites W2097274806 @default.
- W1973020270 cites W2107316430 @default.
- W1973020270 cites W2116958131 @default.
- W1973020270 cites W2126671525 @default.
- W1973020270 cites W2139281024 @default.
- W1973020270 cites W2143128079 @default.
- W1973020270 cites W2157583759 @default.
- W1973020270 cites W2162129176 @default.
- W1973020270 cites W2166417397 @default.
- W1973020270 cites W2166777744 @default.
- W1973020270 cites W2170709362 @default.
- W1973020270 cites W2908613460 @default.
- W1973020270 doi "https://doi.org/10.1130/0016-7606(2001)113<1025:slhboi>2.0.co;2" @default.
- W1973020270 hasPublicationYear "2001" @default.
- W1973020270 type Work @default.
- W1973020270 sameAs 1973020270 @default.
- W1973020270 citedByCount "17" @default.
- W1973020270 countsByYear W19730202702012 @default.
- W1973020270 countsByYear W19730202702013 @default.
- W1973020270 countsByYear W19730202702015 @default.
- W1973020270 crossrefType "journal-article" @default.
- W1973020270 hasAuthorship W1973020270A5006685240 @default.
- W1973020270 hasAuthorship W1973020270A5089544871 @default.
- W1973020270 hasConcept C111368507 @default.
- W1973020270 hasConcept C115880899 @default.
- W1973020270 hasConcept C127313418 @default.
- W1973020270 hasConcept C151730666 @default.
- W1973020270 hasConcept C161191863 @default.
- W1973020270 hasConcept C166957645 @default.
- W1973020270 hasConcept C2778805511 @default.
- W1973020270 hasConcept C32277403 @default.
- W1973020270 hasConcept C41008148 @default.
- W1973020270 hasConcept C95457728 @default.
- W1973020270 hasConceptScore W1973020270C111368507 @default.
- W1973020270 hasConceptScore W1973020270C115880899 @default.
- W1973020270 hasConceptScore W1973020270C127313418 @default.
- W1973020270 hasConceptScore W1973020270C151730666 @default.
- W1973020270 hasConceptScore W1973020270C161191863 @default.
- W1973020270 hasConceptScore W1973020270C166957645 @default.
- W1973020270 hasConceptScore W1973020270C2778805511 @default.
- W1973020270 hasConceptScore W1973020270C32277403 @default.
- W1973020270 hasConceptScore W1973020270C41008148 @default.
- W1973020270 hasConceptScore W1973020270C95457728 @default.
- W1973020270 hasIssue "8" @default.
- W1973020270 hasLocation W19730202701 @default.
- W1973020270 hasOpenAccess W1973020270 @default.
- W1973020270 hasPrimaryLocation W19730202701 @default.
- W1973020270 hasRelatedWork W163493885 @default.
- W1973020270 hasRelatedWork W1998854056 @default.
- W1973020270 hasRelatedWork W2027986338 @default.
- W1973020270 hasRelatedWork W2032291131 @default.
- W1973020270 hasRelatedWork W2240559228 @default.
- W1973020270 hasRelatedWork W2391625088 @default.
- W1973020270 hasRelatedWork W2755812209 @default.
- W1973020270 hasRelatedWork W3013225796 @default.