Abstract

Research Article| January 01, 2004 Reply M. Elliot Smith; M. Elliot Smith 1University of Wisconsin—Madison, Geology and Geophysics, 1215 West Dayton Street, Madison, Wisconsin 53703, USA Search for other works by this author on: GSW Google Scholar Brad S. Singer; Brad S. Singer 1University of Wisconsin—Madison, Geology and Geophysics, 1215 West Dayton Street, Madison, Wisconsin 53703, USA Search for other works by this author on: GSW Google Scholar Alan R. Carroll Alan R. Carroll 1University of Wisconsin—Madison, Geology and Geophysics, 1215 West Dayton Street, Madison, Wisconsin 53703, USA Search for other works by this author on: GSW Google Scholar GSA Bulletin (2004) 116 (1-2): 253–256. https://doi.org/10.1130/B25491R.1 Article history received: 11 Sep 2003 accepted: 11 Sep 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 M. Elliot Smith, Brad S. Singer, Alan R. Carroll; Reply. GSA Bulletin 2004;; 116 (1-2): 253–256. doi: https://doi.org/10.1130/B25491R.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 In their comment, Clyde et al. point out an important discrepancy between our 40Ar/39Ar-based age model (Smith et al., 2003), paleomagnetic stratigraphy (Clyde et al., 1997; 2001), and an 40Ar/39Ar age from Murphey et al. (1999). Specifically, Clyde et al. conclude that the F+ chron within the Bridger Formation at the top of their South Pass section (Clyde et al., 2001) correlates to C22n instead of C21n, implying that the entire Green River Formation is contained between C23r and C22r. Their interpretation is based largely on... You do not have access to this content, please speak to your institutional administrator if you feel you should have access.

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