Analysis of subsurface structures based on seismic and gravimetric exploration methods in the Las Tres Vírgenes volcanic complex and geothermal field, Baja California Sur, Mexico
| Autor: | K.L. Casallas-Moreno, C.A. Gallegos-Castillo, E. Gómez-Arias, Mario González-Escobar, Antonio González-Fernández, E.A. Mastache-Román |
|---|---|
| Rok vydání: | 2021 |
| Předmět: |
geography
geography.geographical_feature_category Renewable Energy Sustainability and the Environment 0211 other engineering and technologies Geochemistry Geology 02 engineering and technology 010502 geochemistry & geophysics Geotechnical Engineering and Engineering Geology 01 natural sciences Cretaceous Volcanic rock Basement (geology) Volcano Gravimetric analysis Sedimentary rock 021108 energy Transect Geothermal gradient 0105 earth and related environmental sciences |
| Zdroj: | Geothermics. 92:102026 |
| ISSN: | 0375-6505 |
| DOI: | 10.1016/j.geothermics.2020.102026 |
| Popis: | Las Tres Virgenes Geothermal Field (LTVGF) is located in the northern flank of the Volcanic Complex (LTVVC) of the same name. The area sits on the northeast part of Baja California Sur, Mexico. The LTVGF is one of five active geothermal fields in the country. It started producing electrical energy in 2001 and currently has an installed capacity of 10 MW. The fluids in the geothermal field circulate through faults and fractures that cut and transect the Cretaceous granodioritic basement and uppermost sedimentary and volcanic rocks. This study presents new seismic (controlled source) and gravimetric models to characterize the structural system of the volcanic complex, its relationship with the movement of geothermal fluids, and the location of new areas with geothermal potential. The seismic sections were correlated with lithological columns from geothermal drill hole. The multichannel analysis of surface waves (MASW) method was used to characterize the shallow ( |
| Databáze: | OpenAIRE |
| Externí odkaz: |
|
Full Text from ScienceDirect