Calculated heat flow for the ensenada region, Baja California, Mexico
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| Format: | Artículo científico |
| Sprache: | en |
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Universidad Autónoma de Baja California
2001
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| author | José María Beltrán Abaunza |
| author_facet | José María Beltrán Abaunza |
| contents | Calculated heat flow for the ensenada region, Baja California, Mexico José María Beltrán Abaunza Ana Luz Quintanilla Montoya Ciencias de la Tierra Mexico heat flow geothermometry Baja California geothermal resource Due to the scarcity of heat flow data in the region of Ensenada, Baja California (Mexico), the presentstudy calculated them using the silica geothermometer technique. The average heat flow valuedetermined was 123.33 ± 35.57 mW m2 (2.95 ± 0.85 HFU). Four zones within the study area, related tothe main fault systems of the region, were found to have high hydrothermal activity. The potential use ofgeothermal resources in the area is feasible as it is considered a low geothermal system with watertemperature values, above the static water level, that vary from 30ºC to 108ºC. 2001 artículo científico 0185-3880 https://www.redalyc.org/articulo.oa?id=48027408 en http://www.redalyc.org/revista.oa?id=480 Ciencias Marinas application/pdf Universidad Autónoma de Baja California Ciencias Marinas (México) Num.4 Vol.27 |
| format | Artículo científico |
| id | redalyc_48027408 |
| institution | Redalyc |
| language | en |
| publishDate | 2001 |
| publisher | Universidad Autónoma de Baja California |
| spellingShingle | Calculated heat flow for the ensenada region, Baja California, Mexico José María Beltrán Abaunza Ciencias de la Tierra Mexico heat flow geothermometry Baja California geothermal resource Calculated heat flow for the ensenada region, Baja California, Mexico José María Beltrán Abaunza Ana Luz Quintanilla Montoya Ciencias de la Tierra Mexico heat flow geothermometry Baja California geothermal resource Due to the scarcity of heat flow data in the region of Ensenada, Baja California (Mexico), the presentstudy calculated them using the silica geothermometer technique. The average heat flow valuedetermined was 123.33 ± 35.57 mW m2 (2.95 ± 0.85 HFU). Four zones within the study area, related tothe main fault systems of the region, were found to have high hydrothermal activity. The potential use ofgeothermal resources in the area is feasible as it is considered a low geothermal system with watertemperature values, above the static water level, that vary from 30ºC to 108ºC. 2001 artículo científico 0185-3880 https://www.redalyc.org/articulo.oa?id=48027408 en http://www.redalyc.org/revista.oa?id=480 Ciencias Marinas application/pdf Universidad Autónoma de Baja California Ciencias Marinas (México) Num.4 Vol.27 |
| title | Calculated heat flow for the ensenada region, Baja California, Mexico |
| topic | Ciencias de la Tierra Mexico heat flow geothermometry Baja California geothermal resource |
| url | https://www.redalyc.org/articulo.oa?id=48027408 |