Eastern Kentucky University Encompass EKU Faculty and Staff choS larship 10-2006 Petrogenesis and tectonic setting of the peralkaline Pine Canyon caldera, Trans-Pecos Texas, USA. John C. White Eastern Kentucky University,
[email protected] Christian S. Benker Eastern Kentucky University Minghua Ren University of Texas at El Paso Kevin M. Urbanczyk Sul Ross State University Don W. Corrick Big Bend National Park Follow this and additional works at: http://encompass.eku.edu/fs_research Part of the Geology Commons, and the Tectonics and Structure Commons Recommended Citation White, J.C., Benker, S.C., Ren, M., Urbanczyk, K.M., and Corrick, D.W., 2006, Petrogenesis and tectonic setting of the peralkaline Pine Canyon caldera, Trans-Pecos Texas, USA. In: Peralkaline Rocks: A Special Issue Dedicated to Henning Sørensen, PERALK2005 Workshop (G. Markl, Ed.) Lithos, v. 91, p. 74-94. (doi: 10.1016.j.lithos.2006.03.015) This Article is brought to you for free and open access by Encompass. It has been accepted for inclusion in EKU Faculty and Staff choS larship by an authorized administrator of Encompass. For more information, please contact
[email protected]. Lithos 91 (2006) 74–94 www.elsevier.com/locate/lithos Petrogenesis and tectonic setting of the peralkaline Pine Canyon caldera, Trans-Pecos Texas, USA ⁎ John Charles White a, , S. Christian Benker a, Minghua Ren b, Kevin M. Urbanczyk c, Donald W. Corrick d a Department of Earth Sciences, Eastern Kentucky University, Richmond, KY 40475, USA b Department of Geological Sciences, University of Texas at El Paso, El Paso, TX 79968, USA c Department of Earth and Physical Sciences, Sul Ross State University, Alpine, TX 79832, USA d National Park Service, Big Bend National Park, TX 79834, USA Received 4 July 2005; accepted 13 March 2006 Available online 19 May 2006 Abstract The Pine Canyon caldera is a small (6–7 km diameter) ash-flow caldera that erupted peralkaline quartz trachyte, rhyolite, and high-silica rhyolite lavas and ash-flow tuffs about 33–32 Ma.