Research Article| June 01, 2003 Dubious case for slab melting in the Northern volcanic zone of the Andes Jennifer M. Garrison; Jennifer M. Garrison 1Department of Earth and Space Sciences, University of California, Los Angeles, California 90095, USA Search for other works by this author on: GSW Google Scholar Jon P. Davidson Jon P. Davidson 2Department of Geological Sciences, University of Durham, South Road, Durham DH1 3LE, UK Search for other works by this author on: GSW Google Scholar Author and Article Information Jennifer M. Garrison 1Department of Earth and Space Sciences, University of California, Los Angeles, California 90095, USA Jon P. Davidson 2Department of Geological Sciences, University of Durham, South Road, Durham DH1 3LE, UK Publisher: Geological Society of America Received: 17 Dec 2002 Revision Received: 19 Feb 2003 Accepted: 21 Feb 2003 First Online: 02 Jun 2017 Online ISSN: 1943-2682 Print ISSN: 0091-7613 Geological Society of America Geology (2003) 31 (6): 565–568. https://doi.org/10.1130/0091-7613(2003)031<0565:DCFSMI>2.0.CO;2 Article history Received: 17 Dec 2002 Revision Received: 19 Feb 2003 Accepted: 21 Feb 2003 First Online: 02 Jun 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn Email Permissions Search Site Citation Jennifer M. Garrison, Jon P. Davidson; Dubious case for slab melting in the Northern volcanic zone of the Andes. Geology 2003;; 31 (6): 565–568. doi: https://doi.org/10.1130/0091-7613(2003)031<0565:DCFSMI>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 SocietyGeology Search Advanced Search Abstract It was first suggested by R.W. Kay that adakites may represent melts of subducted slab: since then, the term adakite has become synonymous with slab melts based on their unusual geochemical signature. This contribution, using the Northern volcanic zone of the Andes as an example, aims (1) to expose the weakness in simply associating a geochemical signature with a genetic mechanism and (2) to underline the importance of using several integrated lines of evidence in assessing the viability of slab melting. We conclude that although slab melting probably occurs in some arcs, regional geochemical trends in the Northern volcanic zone and their relationship to the subduction-zone architecture are not indicative of slab melting and can be accounted for by normal arc magmatic processes acting on wedge-derived basaltic magmas. You do not have access to this content, please speak to your institutional administrator if you feel you should have access.
No takes yet. Share an insight, caveat, or question.
Garrison et al. (2003) studied this question.
Synapse has enriched 5 related papers. Consider them for comparative context: