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• W2149173837 abstract "Research Article| February 01, 2005 Evaluating slab-plate coupling in the Indo-Australian plate Mike Sandiford; Mike Sandiford 1School of Earth Sciences, University of Melbourne, Melbourne, VIC 3010, Australia Search for other works by this author on: GSW Google Scholar David Coblentz; David Coblentz 2Los Alamos National Laboratory, Los Alamos, New Mexico, New Mexico 87545, USA Search for other works by this author on: GSW Google Scholar Wouter Pieter Schellart Wouter Pieter Schellart 3Research School of Earth Sciences, Australian National University, Canberra, ACT 0200, Australia Search for other works by this author on: GSW Google Scholar Geology (2005) 33 (2): 113–116. https://doi.org/10.1130/G20898.1 Article history received: 08 Jun 2004 rev-recd: 06 Oct 2004 accepted: 07 Oct 2004 first online: 09 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share MailTo Twitter LinkedIn Tools Icon Tools Get Permissions Search Site Citation Mike Sandiford, David Coblentz, Wouter Pieter Schellart; Evaluating slab-plate coupling in the Indo-Australian plate. Geology 2005;; 33 (2): 113–116. doi: https://doi.org/10.1130/G20898.1 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 Distributed seismicity in the central Indian Ocean affords a unique opportunity to evaluate the extent of slab-plate coupling in the Indo-Australian plate. The mix of reverse-fault and strike-slip mechanisms in this region, with northwest-southeast to north-south maximum horizontal stress, SHmax, implies that the effective slab pull is no more than ∼10% of the total negative buoyancy operating on the subducting slab. Numerical models of the intraplate stress field predict a slab-pull component along the Sumatra and Java boundary segments of 2.82 ± 0.82 and 0.89 ± 0.35 × 1012 N·m−1, respectively. Mantle tomographic constraints coupled with insights from analogue modeling suggest that the differences relate to variations in the depth extent of the slabs and the degree of slab support provided by the transition zone. These results help resolve apparent contradictions between insights from intraplate stress fields and plate dynamics; i.e., although plate motion is dominated by subduction, slab pull is only poorly expressed in the intraplate stress field because of low slab-plate coupling. 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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• W2149173837 title "Evaluating slab-plate coupling in the Indo-Australian plate" @default.
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