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Hydrothermal-flow regime and magmatic heat source of the Cerro Prieto geothermal system, Baja California, Mexico
Our detailed three-dimensional model of the natural flow regime of the Cerro Prieto geothermal field, before steam production began, i s based on p a tterns of hydrothermal mineral zones and l i g h t stable isotopic ratios observed i n rock samples from more t h a n f i f t y deep wells, together w i t h temperature gradients, wireline logs and other data. A t the level so far penetrated by drilling, this hydrothermal system was heated by a thermal plume of water close t o boiling, inclined adoi:10.2172/5877114 fatcat:pbtx5kbrmndlzhmex5k5fltiem