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• W2128952208 abstract "Research Article| May 01, 2008 Cracking of lithosphere north of the Galapagos triple junction Hans Schouten; Hans Schouten 1Department of Geology and Geophysics, Woods Hole Oceanographic Institution, Woods Hole, Massachusetts 02543, USA Search for other works by this author on: GSW Google Scholar Deborah K. Smith; Deborah K. Smith 1Department of Geology and Geophysics, Woods Hole Oceanographic Institution, Woods Hole, Massachusetts 02543, USA Search for other works by this author on: GSW Google Scholar Laurent G.J. Montési; Laurent G.J. Montési 2Department of Geology, University of Maryland, College Park, Maryland 20742, USA Search for other works by this author on: GSW Google Scholar Wenlu Zhu; Wenlu Zhu 2Department of Geology, University of Maryland, College Park, Maryland 20742, USA Search for other works by this author on: GSW Google Scholar Emily M. Klein Emily M. Klein 3Division of Earth and Ocean Sciences, Duke University, Durham, North Carolina 27708, USA Search for other works by this author on: GSW Google Scholar Geology (2008) 36 (5): 339–342. https://doi.org/10.1130/G24431A.1 Article history received: 05 Oct 2007 rev-recd: 21 Dec 2007 accepted: 01 Jan 2008 first online: 02 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 Hans Schouten, Deborah K. Smith, Laurent G.J. Montési, Wenlu Zhu, Emily M. Klein; Cracking of lithosphere north of the Galapagos triple junction. Geology 2008;; 36 (5): 339–342. doi: https://doi.org/10.1130/G24431A.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 Galapagos triple junction is a ridge-ridge-ridge triple junction where the Cocos, Nazca, and Pacific plates meet around the Galapagos microplate. Directly north of the large scarps of the Cocos-Nazca Rift, a 250-km-long and 50-km-wide band of northwest-southeast–trending cracks with volcanics at their western ends crosscuts and blankets the north-south–trending abyssal hills of the East Pacific Rise. It appears that the roughly northeast-southwest extension of East Pacific Rise–generated seafloor has been accommodated by a succession of minor rifts that, during at least the past 4 m.y., had their triple junctions with the East Pacific Rise at distances of 50–100 km north of the tip of the propagating Cocos-Nazca Rift. We propose that the rift locations are controlled by stresses associated with the dominant Cocos-Nazca Rift, and scaled by the distance of its tip to the East Pacific Rise. We speculate that similar ephemeral rifts occurred south of the Cocos-Nazca Rift and were instrumental in the origin of the rotating Galapagos microplate ca. 1.5 Ma. 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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• W2128952208 title "Cracking of lithosphere north of the Galapagos triple junction" @default.
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