Research Article| July 01, 2008 Geodynamic significance of S-type granites in circum-Pacific orogens W.J. Collins; W.J. Collins 1School of Earth and Environmental Sciences, James Cook University, Townsville, Queensland 4814, Australia Search for other works by this author on: GSW Google Scholar S.W. Richards S.W. Richards 2Research School of Earth Sciences, Australian National University, Canberra 0200, Australia Search for other works by this author on: GSW Google Scholar Author and Article Information W.J. Collins 1School of Earth and Environmental Sciences, James Cook University, Townsville, Queensland 4814, Australia S.W. Richards 2Research School of Earth Sciences, Australian National University, Canberra 0200, Australia Publisher: Geological Society of America Received: 29 Nov 2007 Revision Received: 04 Apr 2008 Accepted: 09 Apr 2008 First Online: 02 Mar 2017 Online ISSN: 1943-2682 Print ISSN: 0091-7613 © 2008 Geological Society of America Geology (2008) 36 (7): 559–562. https://doi.org/10.1130/G24658A.1 Article history Received: 29 Nov 2007 Revision Received: 04 Apr 2008 Accepted: 09 Apr 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 W.J. Collins, S.W. Richards; Geodynamic significance of S-type granites in circum-Pacific orogens. Geology 2008;; 36 (7): 559–562. doi: https://doi.org/10.1130/G24658A.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 In Phanerozoic circum-Pacific orogenic belts, most “post-collisional” S-type granites and associated high-temperature, low-pressure metamorphic complexes formed during early arc extension. The granites are part of a tripartite association consisting of (1) inboard S-type granite, (2) outboard oceanic arc, and (3) intervening, turbidite-filled backarc basin. S-type granites herald the formation of new outboard oceanic arc and extensional backarc systems, but thickening of a preexisting, sediment-dominated back-arc basin is a prerequisite for their generation. In these environments, S-type plutonism is triggered by renewal of arc magmatism following thickening, when hot basaltic magmas are intruded into the thickened backarc crust once slab retreat is reestablished. With ongoing extension during retreat, the crust becomes progressively thinned, the sedimentary contribution is diminished, and the granites lose their S-type character. Such tripartite associations involving S-type granite are probably diagnostic of repeated slab-retreat episodes, and the Jurassic U.S. cordillera might be an example. You do not have access to this content, please speak to your institutional administrator if you feel you should have access.