Generation and evolution of hydrothermal fluids at Yellowstone: Insights from the Heart Lake Geyser Basin
Article first published online: 28 JAN 2012
This paper is not subject to U.S. copyright. Published in 2012 by the American Geophysical Union
Geochemistry, Geophysics, Geosystems
Volume 13, Issue 1, January 2012
How to Cite
2012), Generation and evolution of hydrothermal fluids at Yellowstone: Insights from the Heart Lake Geyser Basin, Geochem. Geophys. Geosyst., 13, Q01017, doi:10.1029/2011GC003835., , , and (
- Issue published online: 28 JAN 2012
- Article first published online: 28 JAN 2012
- Manuscript Accepted: 20 DEC 2011
- Manuscript Revised: 15 DEC 2011
- Manuscript Received: 15 AUG 2011
Auxiliary material for this article contains a ternary diagram showing He, CH4 and Ar relations for gas collected from fumaroles and frying pans.
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|ggge2097-sup-0002-fs01.pdf||PDF document||137K||Figure S1. Ternary diagram showing He, CH4 and Ar relations for gas collected from fumaroles and frying pans demonstrates that Yellowstone gases can be discriminated by their CH4/He ratios, that discrete geographic areas have unique CH4/He ratios, and that most groups form an array of mixtures of magmatic and crustal gases with those derived from boiling of meteoric waters (Ar end-member).|
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|ggge2097-sup-0004-t02.txt||plain text document||2K||Tab-delimited Table 2.|
|ggge2097-sup-0005-t03.txt||plain text document||1K||Tab-delimited Table 3.|
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