Structural and sedimentological study of the Cerro Prieto geothermal field, Baja California, Mexico [electronic resource]

Geophysical and lithologic well logs from over fifty wells have been qualitatively and quantitatively analyzed using both manual and computer interpretation techniques. These logs were studied to make stratigraphic correlations throughout the Cerro Prieto field and to interpret the deltaic depositio...

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Bibliographic Details
Online Access: Online Access
Corporate Authors: Lawrence Berkeley Laboratory (Researcher), Lawrence Berkeley National Laboratory (Researcher)
Format: Government Document Electronic eBook
Language:English
Published: Berkeley, Calif. : Oak Ridge, Tenn. : Lawrence Berkeley National Laboratory ; distributed by the Office of Scientific and Technical Information, U.S. Dept. of Energy, 1981.
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MARC

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245 0 0 |a Structural and sedimentological study of the Cerro Prieto geothermal field, Baja California, Mexico  |h [electronic resource] 
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500 |a AAPG-SEPM-EMD annual convention, Denver, CO, USA, 8 Jun 1980. 
500 |a Vonder Haar, S. 
520 3 |a Geophysical and lithologic well logs from over fifty wells have been qualitatively and quantitatively analyzed using both manual and computer interpretation techniques. These logs were studied to make stratigraphic correlations throughout the Cerro Prieto field and to interpret the deltaic depositional environment of the field's lithologic units. Dipmeter and seismic data were of great value in making stratigraphic interpretations and extrapolations. Cross sections were constructed to illustrate lithofacies variations throughout the geothermal field. In turn, these sections were used to construct a three-dimensional model of the Cerro Prieto geothermal reservoir. Petrographic microscopy, scanning electron microscopy, and x-ray diffraction analyses of well-bore cuttings and cores were utilized to determine the degree and distribution of hydrothermal alteration by fluids at temperatures up to 350°C, the origins of dissolution porosity, and the relative degree of fracture versus dissolution porosity. The results of these analyses were confirmed by log-derived determinations of formation fluid properties, porosity, and petrophysical properties and by studies of Cerro Prieto cores conducted under in-situ conditions. The results of this research were integrated into the Cerro Prieto reservoir model. 
520 0 |a Geothermal Legacy. 
536 |b W-7405-ENG-48. 
650 7 |a Stratigraphy.  |2 local. 
650 7 |a Gamma-gamma Logging.  |2 local. 
650 7 |a Drill Cores.  |2 local. 
650 7 |a Porosity.  |2 local. 
650 7 |a Developing Countries.  |2 local. 
650 7 |a Geology.  |2 local. 
650 7 |a Sediments.  |2 local. 
650 7 |a Well Logging.  |2 local. 
650 7 |a Geologic Structures.  |2 local. 
650 7 |a North America.  |2 local. 
650 7 |a Mexico.  |2 local. 
650 7 |a Latin America.  |2 local. 
650 7 |a Radioactivity Logging.  |2 local. 
650 7 |a Maps.  |2 local. 
650 7 |a Cerro Prieto Geothermal Field.  |2 local. 
650 7 |a Geothermal Fields.  |2 local. 
650 7 |a Lithology.  |2 local. 
650 7 |a Geothermal Energy.  |2 edbsc. 
710 2 |a Lawrence Berkeley Laboratory.  |4 res. 
710 2 |a Lawrence Berkeley National Laboratory.  |4 res. 
710 1 |a United States.  |b Department of Energy.  |b Office of Scientific and Technical Information.  |4 dst. 
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