Tectonic-magmatic-hydrothermal interactions in a hot dry rock geothermal system: The role of the transfer and normal faults in the Acoculco caldera (Mexico)

Liotta, Domenico; Brogi, Andrea; Wheeler, Walter H.; Bastensen, Eivind; Garduño-Monroy, Victor Hugo; Macias, José Luis; Sosa-Ceballos, Giovanni; Pola, Antonio; Avellán, Denis-Ramón; Bianco, Caterina; Olvera-García, Emmanuel; Gómez-Alvarez, Fidel; Israde-Alcantara, Isabel; Jiménez-Haro, Adrian; Piccardi, Luigi; Zucchi, Martina

doi:10.1016/j.jvolgeores.2023.107963

Journal of Volcanology and Geothermal Research

2023

DOI: 10.1016/j.jvolgeores.2023.107963

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Tectonic-magmatic-hydrothermal interactions in a hot dry rock geothermal system: The role of the transfer and normal faults in the Acoculco caldera (Mexico)

Domenico Liotta,

Andrea Brogi,

Walter H. Wheeler

et al.

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2024

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Cited by 3 publications

References 64 publications

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Soil CO2 fluxes measured in the Acoculco Geothermal System, Mexico: Baseline emissions from a long-term prospection programme

Pérez-Zárate,

Santoyo,

Jácome-Paz

et al. 2024

Geochemistry

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Soil CO2 fluxes measured in the Acoculco Geothermal System, Mexico: Baseline emissions from a long-term prospection programme

Pérez-Zárate,

Santoyo,

Jácome-Paz

et al. 2024

Geochemistry

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The difference in hydrochemical characteristics of geothermal water between the eastern and western parts of the Wugongshan area and its genetic mechanism

Jia,

Liu,

Yan

et al. 2024

Journal of Geochemical Exploration

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Análisis morfo-estructural del Campo Volcánico Monogenético Guamuéz-Sibundoy (sur de Colombia)

Murillo-Orobio,

Chapuel-Cuasapud,

Botero-Gómez

et al. 2024

Geofis Int

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El Campo Volcánico Monogenético Guamuéz-Sibundoy (CVMGS) está localizado en los Andes del Norte, sur de Colombia, en una depresión geomorfológica que se conoce como Valle de Sibundoy. Esta zona se encuentra influenciada por un conjunto de fallas relacionadas con el Sistema de Fallas de Algeciras. Con el objetivo de comprender la actividad tectónica registrada en los rasgos morfo-estructurales y la interacción con el CVMGS, se presenta una caracterización morfo-estructural a través del procesamiento de modelos digitales usando sistemas de información geográfica (SIG). Para esto, utilizando un modelo de elevación digital, se analizaron las pendientes, los drenajes, un mapa de aspectos y los lineamientos sobre un relieve sombreado, y se identificaron deflexiones en ríos y segmentos rectilíneos. El análisis evidencia que la concentración de lineamientos presentes en la zona de estudio puede relacionarse con zonas de daño de las fallas principales, con patrones de dirección WNW-ESE, NW-SE, NNE-SSW y NE-SW. Los lineamientos en sentido WNW-ESE y NW-SE se relacionan con la falla Sibundoy y el Sistema de Fallas de Algeciras, mientras que los lineamientos en sentido NNE-SSW y NE-SW con la falla San Francisco-Yunguillo. Los resultados permiten evidenciar fallas regionales que no han sido registradas en la literatura, así como proponer un modelo estructural basado en estos sistemas y la interacción con fallas transversales.

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Tectonic-magmatic-hydrothermal interactions in a hot dry rock geothermal system: The role of the transfer and normal faults in the Acoculco caldera (Mexico)

Cited by 3 publications

References 64 publications

Soil CO2 fluxes measured in the Acoculco Geothermal System, Mexico: Baseline emissions from a long-term prospection programme

Soil CO2 fluxes measured in the Acoculco Geothermal System, Mexico: Baseline emissions from a long-term prospection programme

The difference in hydrochemical characteristics of geothermal water between the eastern and western parts of the Wugongshan area and its genetic mechanism

Análisis morfo-estructural del Campo Volcánico Monogenético Guamuéz-Sibundoy (sur de Colombia)

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