Hydrogeochemical data for thermal and nonthermal waters and gases of the Valles Caldera- southern Jemez Mountains region, New Mexico
Author(s) -
Lisa Shevenell,
Fraser Goff,
F. Vuataz,
P.E. Trujillo,
D. Counce,
C.J. Janik,
W. Evans
Publication year - 1987
Language(s) - English
Resource type - Reports
DOI - 10.2172/6729933
Subject(s) - caldera , geology , geothermal gradient , geochemistry , volcano , meteoric water , hydrothermal circulation , sulfate , geomorphology , paleontology , chemistry , organic chemistry
This report presents field, chemical, gas, and isotopic data for thermal and nonthermal waters of the southern Jemez Mountains, New Mexico. This region includes all thermal and mineral waters associated with Valles Caldera and many of those located near the Nacimiento Uplift, north of San Ysidro. Waters of the region can be categorized into five general types: (1) surface and near-surface meteoric waters; (2) acid-sulfate waters at Sulphur Springs (Valles Caldera); (3) thermal meteoric waters in the ring fracture zone (Valles Caldera); (4) deep geothermal waters of the Baca geothermal field and derivative waters in the Soda Dam and Jemez Springs area (Valles Caldera); and (5) mineralized waters near San Ysidro. Some waters display chemical and isotopic characteristics intermediate between the types listed. Data in this report will help in interpreting the geothermal potential of the Jemez Mountains region and will provide background for investigating problems in hydrology, structural geology, hydrothermal alterations, and hydrothermal solution chemistry.
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