| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 5446820 | Energy Procedia | 2016 | 8 Pages |
Abstract
The main geothermal reservoir is located within the fractured Pre-Palaeozoic-Ordovician units. The reservoir is recharged by meteoric waters. Geothermal fluids upwell where main regional structures intersect secondary structures associated with the development of the Tocomar basin. Preliminary data indicate a reservoir temperature of ⼠200° C and a local geothermal gradient of ⼠130° C/km associated with the Quaternary volcanic activity in the Tocomar area.
Related Topics
Physical Sciences and Engineering
Energy
Energy (General)
Authors
G. Giordano, F. Ahumada, L. Aldega, W. Baez, R. Becchio, S. Bigi, C. Caricchi, A. Chiodi, S. Corrado, A.A. De Benedetti, A. Favetto, R. Filipovich, A. Fusari, G. Groppelli, C. Invernizzi, R. Maffucci, G. Norini, A. Pinton, J. Viramonte,