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• W2322045914 abstract "Research Article| December 01, 2011 Continental exhumation triggered by partial melting at ultrahigh pressure L. Labrousse; L. Labrousse 1UPMC U. Paris 6, ISTeP, F-75005 Paris, France2CNRS, UMR 7193, F-75005 Paris, France Search for other works by this author on: GSW Google Scholar G. Prouteau; G. Prouteau 3ISTO, UMR 6113, CNRS/U. Orléans, 1A rue de la Férollerie, F-45071 Orleans, France Search for other works by this author on: GSW Google Scholar A.-C. Ganzhorn A.-C. Ganzhorn 1UPMC U. Paris 6, ISTeP, F-75005 Paris, France2CNRS, UMR 7193, F-75005 Paris, France Search for other works by this author on: GSW Google Scholar Author and Article Information L. Labrousse 1UPMC U. Paris 6, ISTeP, F-75005 Paris, France2CNRS, UMR 7193, F-75005 Paris, France G. Prouteau 3ISTO, UMR 6113, CNRS/U. Orléans, 1A rue de la Férollerie, F-45071 Orleans, France A.-C. Ganzhorn 1UPMC U. Paris 6, ISTeP, F-75005 Paris, France2CNRS, UMR 7193, F-75005 Paris, France Publisher: Geological Society of America Received: 05 Apr 2011 Revision Received: 20 Jul 2011 Accepted: 03 Aug 2011 First Online: 09 Mar 2017 Online ISSN: 1943-2682 Print ISSN: 0091-7613 © 2011 Geological Society of America Geology (2011) 39 (12): 1171–1174. https://doi.org/10.1130/G32316.1 Article history Received: 05 Apr 2011 Revision Received: 20 Jul 2011 Accepted: 03 Aug 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 L. Labrousse, G. Prouteau, A.-C. Ganzhorn; Continental exhumation triggered by partial melting at ultrahigh pressure. Geology 2011;; 39 (12): 1171–1174. doi: https://doi.org/10.1130/G32316.1 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 Partial melting textures, observed in most continental crust buried in ultrahigh-pressure (UHP) conditions, have mostly been related to their retrograde evolution during exhumation in collisional orogens. Analysis of leucosomes from the Western Gneiss Region (WGR, Norway) UHP and HP domains in the Caledonides show a wide scatter of their chemistries, from early ones close to trondhjemites restricted to UHP domains, to granites in late occurrences or associated with HP domains. Nearly trondhjemitic compositions compare with hydrous melts produced in felsic systems at high pressure (>2 GPa) and moderate temperature (<900 °C). Partial melting experiments at higher temperatures or in dry conditions produce granitic glasses similar to late leucosomes from the WGR. Comparison of pressure-temperature paths for Caledonian eclogites with melting and dehydration reactions for the surrounding gneiss suggest that (1) the continental crust remained partially hydrated during its subduction to ultrahigh pressure, and (2) partial melting reactions producing the trondhjemitic melts started as soon as the WGR rocks reached their hydrated solidus, at the peak pressure recorded by the eclogites. The limited partial melting degree at the peak conditions induced weakening of the continental crust, decoupling from the lithospheric root, and initiation of exhumation. 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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