skip to main content
OSTI.GOV title logo U.S. Department of Energy
Office of Scientific and Technical Information

Title: Model for the heat source of the Cerro Prieto magma-hydrothermal system, Baja California, Mexico

Technical Report ·
DOI:https://doi.org/10.2172/5791458· OSTI ID:5791458

Earlier studies at Cerro Prieto led to the development of a qualitative model for fluid flow in the geothermal system before it was drilled and perturbed by production. Current efforts are directed towards numerical modeling of heat and mass transfer in the system in this undisturbed state. This one-dimensional model assumes that the heat source was a single basalt/gabbro intrusion which provided heat to the system as it cooled. After compilation of various information of the physical properties of the reservoir, the enthalpy contained in two 1 cm thick sections across the reservoir orthogonal to each other was calculated. Various shapes, sizes and depths for the intrusion were considered as initial conditions and boundary conditions for the calculations of heat transfer. A family of numerical models which so far gives the best matches to the conditions observed in the field today have in common a funnel-shaped intrusion with a top 4 km wide emplaced at a depth of 5 km some 30,000 to 50,000 years ago, providing heat to the geothermal system.

Research Organization:
California Univ., Riverside (USA). Inst. of Geophysics and Planetary Physics; Arizona Univ., Tucson (USA). Dept. of Geosciences
DOE Contract Number:
FC07-80ID12145
OSTI ID:
5791458
Report Number(s):
DOE/ID/12145-T1; ON: DE83016670
Resource Relation:
Other Information: Portions are illegible in microfiche products
Country of Publication:
United States
Language:
English