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Research Article| August 01, 2003 Reply Dawnika L. Blatter; Dawnika L. Blatter 1Department of Earth and Planetary Science, University of California, Berkeley, California 94720, USA Search for other works by this author on: GSW Google Scholar Ian S.E. Carmichael; Ian S.E. Carmichael 1Department of Earth and Planetary Science, University of California, Berkeley, California 94720, USA Search for other works by this author on: GSW Google Scholar Alan L. Deino; Alan L. Deino 2Berkeley Geochronology Center, 2455 Ridge Road, Berkeley, California 94709, USA Search for other works by this author on: GSW Google Scholar Paul Renne Paul Renne 3Department of Earth and Planetary Science, University of California, Berkeley, California 94720, USA and Berkeley Geochronology Center, 2455 Ridge Road, Berkeley, California 94709, USA Search for other works by this author on: GSW Google Scholar GSA Bulletin (2003) 115 (8): 1021–1024. https://doi.org/10.1130//B25353R.1 Article history received: 11 Mar 2003 accepted: 12 Mar 2003 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 Dawnika L. Blatter, Ian S.E. Carmichael, Alan L. Deino, Paul Renne; Reply. GSA Bulletin 2003;; 115 (8): 1021–1024. doi: https://doi.org/10.1130//B25353R.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 SocietyGSA Bulletin Search Advanced Search We find the comments of Torres-Alvarado and Verma to be tangential to the themes presented in Blatter et al. (2001), and feel that this is yet another effort by Verma and collaborators to refute a subduction-related origin for the Mexican Volcanic Belt; however, we welcome the opportunity to reply with some comments of our own. The purpose of the Blatter et al. (2001) paper was to present the geologic distribution, estimated eruptive volumes, and radiometric ages of Neogene to Quaternary volcanism in the Zitácuaro–Valle de Bravo region of the central Mexican Volcanic Belt. Basic geochemical data, including major elements... You do not have access to this content, please speak to your institutional administrator if you feel you should have access.