Zeolitic Alteration
Relict Geothermal Features
Zeolite minerals, including mordenite and clinoptilolite, have been identified in a number of caldera systems. These and other zeolite minerals are regionally extensive, and their formation is associated with late stage degassing of magmatic fluids and mixing with meteoric water.
Examples
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CSVGeothermal Resource Area | Geothermal Region | Control Structure | Host Rock Age | Host Rock Lithology | Mean Capacity | Mean Reservoir Temp |
---|---|---|---|---|---|---|
Valles Caldera - Redondo Geothermal Area | Rio Grande Rift | Caldera Rim Margins Fault Intersection Stratigraphic Boundaries | Mississippian-Pennsylvanian; Pleistocene, 1.6 to 1.25 Ma | Limestone-Madera Formation “MIPu”; Rhyolitic tuff-Intracaldera Bandelier Tuff (upper Tshirege “Qbt” and lower Otowi “Qbo” members); Caldera Fill Rhyolite (shallow) | ||
Valles Caldera - Sulphur Springs Geothermal Area | Rio Grande Rift | Caldera Rim Margins Fault Intersection Stratigraphic Boundaries | Precambrian; Mississippian-Pennsylvanian; Pleistocene, 1.6 to 1.25 Ma; Pliocene; Miocene | Crystalline basement “pCu”; Limestone-Madera Formation “MIPu”; Rhyolitic tuff-Bandelier Tuff (upper Tshirege “Qbt” and lower Otowi “Qbo” members); Caldera Fill Rhyolite (shallow); Dacitic/Andesitic to Rhyolitic lavas and tuffs-Keres Group Volcanics (shallow); Santa Fe Group volcaniclastics “Tsf” |