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Gas Analysis of Core Samples from Fenton Hill [electronic resource].

Published:
Washington, D.C. : United States. Dept. of Energy, 1983.
Oak Ridge, Tenn. : Distributed by the Office of Scientific and Technical Information, U.S. Dept. of Energy
Physical Description:
5 pages : digital, PDF file
Additional Creators:
Los Alamos National Laboratory, United States. Department of Energy, and United States. Department of Energy. Office of Scientific and Technical Information
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Summary:
Among the suggested sources of the CO2 produced by the deep wells at Fenton Hill are secondary fluid inclusions produced during formation of the magma chamber related to the Valles event. If this hypothesis were correct, the number of fluid inclusions and the amount of CO2 in them should increase with depth in the well bore, particularly since EE-2 was deviated toward the caldera. Twenty core samples and two surface gneiss samples from Guadalupe Box were decrepitated to open these inclusions and the gases analyzed by mass spectrometry by MIDECO of Salt Lake City.
Report Numbers:
E 1.99:la-ur--15-29172-08
la-ur--15-29172-08
Subject(s):
Other Subject(s):
Note:
Published through SciTech Connect.
07/15/1983.
"la-ur--15-29172-08"
A. William Laughlin.
Funding Information:
AC52-06NA25396
View MARC record | catkey: 23778499