Prefeasibility Geothermal Assessment of Platanares, Department of Copan, Honduras.

摘要

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 100C, 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 225C. Three exploration core holes (7.8 cm diameter) have been drilled to a maximum depth of 680 m and maximum temperature of 165C. 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 139C/km at 400 m. Downward continuation of this gradient implies that the minimum depth to the geothermal resource (225C) is 1.5 to 2.0 km. 13 refs., 4 figs.