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36 Cl as a tracer in geothermal systems: Example from Valles Caldera, New Mexico
Author(s) -
Phillips F. M.,
Goff F.,
Vuataz F.,
Bentley H. W.,
Elmore D.,
Gove H. E.
Publication year - 1984
Publication title -
geophysical research letters
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.007
H-Index - 273
eISSN - 1944-8007
pISSN - 0094-8276
DOI - 10.1029/gl011i012p01227
Subject(s) - caldera , geothermal gradient , tracer , geology , chlorine , geochemistry , mineralogy , seismology , volcano , geophysics , nuclear physics , chemistry , physics , organic chemistry
The chlorine‐36 content of three thermal waters from Valles Caldera, New Mexico has been analyzed to investigate the use of chlorine‐36 as a geothermal tracer.
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