Exposed columns in the Valles Caldera ignimbrites as records of hydrothermal cooling, Jemez Mountains, New Mexico, USA

Author:

Self Stephen,Randolph-Flagg Noah,Bailey John E.,Manga Michael

Funder

National Science Foundation

Department of Geology and Geophysics, Yale University

National Aeronautics and Space Administration

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geophysics

Reference82 articles.

1. Geomorphological Evolution of the 1991 Mount Pinatubo Ignimbrite Sheet;Bailey,2001

2. The properties and formation of erosional pipe-shaped structures in ignimbrites around the Valles Caldera;Bailey;Geol. Soc. Amer. Abstracts with Programs,2010

3. Valley Wall Evolution of the Bandelier Ignimbrite; Clues from the 1991 Pinatubo Ignimbrite Sheet. Eos Trans AGU 80(46), fall. Meet. Suppl., Abstract V51B-10;Bailey,1999

4. Pre and Post-eruptive Investigations of Gas and Water Samples from Mount St. Helens, Washington, 2002-2005. USGS Prof. Paper 1750;Bergfeld,2008

5. Summary of the Mineralogy-Petrology of Tuffs of Yucca Mountain and the Secondary-Phase Thermal Stability in Tuffs. Los Alamos National Laboratory Report LA-9321-UC-70;Bish,1982

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