Abstract
Research Article| May 01, 2000 Evolution of Cupido and Coahuila carbonate platforms, Early Cretaceous, northeastern Mexico: Discussion and reply: Discussion David L. Amsbury David L. Amsbury 1128 Homestead, Kerrville, Texas 78028, USA Search for other works by this author on: GSW Google Scholar GSA Bulletin (2000) 112 (5): 799. https://doi.org/10.1130/0016-7606(2000)112<799:EOCACC>2.0.CO;2 Article history received: 19 Jul 1999 accepted: 26 Aug 1999 first online: 01 Jun 2017 Cite View This Citation Add to Citation Manager Share Icon Share Twitter LinkedIn Tools Icon Tools Get Permissions Search Site Citation David L. Amsbury; Evolution of Cupido and Coahuila carbonate platforms, Early Cretaceous, northeastern Mexico: Discussion and reply: Discussion. GSA Bulletin 2000;; 112 (5): 799. doi: https://doi.org/10.1130/0016-7606(2000)112<799:EOCACC>2.0.CO;2 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search nav search search input Search input auto suggest search filter All ContentBy SocietyGSA Bulletin Search Advanced Search The article by Lehmann et al. (1999) is a welcome addition to the literature on Cretaceous rocks of northern Mexico. It contains a wealth of data; the implications for the stratigraphy of Texas and other regions will require time to digest. However, unfortunate terminology in the title and in the paper calls for immediate comment. The Cupido Limestone is a lithofacies of the Coahuila provincial series (Smith, 1970, p. 16–19, and references therein). The Lehman et al. (1999) usage of “Cupido platform” actually means “carbonate rocks formed on the Coahuila platform during the deposition of the Coahuila Series.”... You do not currently have access to this article.
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