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Title: Prefeasibility geothermal assessment of Platanares, Department of Copan, Honduras

Conference ·
OSTI ID:6107042

The Platanares geothermal system is located in a region of active Quaternary tectonism in western Honduras. Although the geothermal area is partially blanketed by Miocene ignimbrites (14.5 m.y.), there are no nearby Quaternary volcanic rocks to act as a young magmatic heat source. No acid-sulfate waters, indicative of vapor-dominated conditions, exist in the area. Hot spring activity is most vigorous along a 2 km stretch of the Quebrada del Agua Caliente fault zone. Natural discharge is high (/approximately/3300 l/min), temperatures range from 35 to 100/degree/C, pH ranges from 7 to 9, and totally dissolved solids are low (/approximately/1100 mg/kg). Chemical geothermometers indicate a subsurface reservoir temperature of about 225/degree/C. Three exploration core holes (7.8 cm diameter) have been drilled to a maximum depth of 680 m and maximum temperature of 165/degree/C. Two holes produce copious amounts of water under artesian conditions (/approximately/500 l/min max; 5 bars flowing) from fractured red beds of Cretaceous to Eocene age (Valle de Angeles Group). Maximum power output is /approximately/4.5 MW (thermal) but CO/sub 2/ released during flashing formed some aragonite scale in one hole. The third core hole has an ''apparent'' conductive gradient of 139/degree/C/km at 400 m. Downward continuation of this gradient implies that the minimum depth to the geothermal resource (225/degree/C) is 1.5 to 2.0 km. 13 refs., 4 figs.

Research Organization:
Los Alamos National Lab., NM (USA)
DOE Contract Number:
W-7405-ENG-36
OSTI ID:
6107042
Report Number(s):
LA-UR-89-1640; CONF-8903134-1; ON: DE89012611
Resource Relation:
Conference: Circum-Pacific energy and minerals conference, San Jose, Costa Rica, 5 Mar 1989; Other Information: Portions of this document are illegible in microfiche products
Country of Publication:
United States
Language:
English