Characterization of the hydrothermal system of the Tinguiririca Volcanic Complex, Central Chile, using structural geology and passive seismic tomography

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dc.contributor.authorPavez, C.
dc.contributor.authorTapia, F.
dc.contributor.authorComte, D.
dc.contributor.authorGutiérrez, F.
dc.contributor.authorLira, E.
dc.contributor.authorCharrier, R.
dc.contributor.authorBenavente, O.
dc.date.accessioned2023-11-22T15:31:27Z
dc.date.available2023-11-22T15:31:27Z
dc.date.issued2016-01
dc.descriptionIndexación: Scopus.es
dc.description.abstractA structural characterization of the hydrothermal–volcanic field associated with the Tinguiririca Volcanic Com plex had been performed by combining passive seismic tomography and structural geology. This complex corre sponds to a 20 km long succession of N25°E oriented of eruptive centers, currently showing several thermal manifestations distributed throughout the area. The structural behavior of this zone is controlled by the El Fierro–El Diablo fault system, corresponding to a high angle reverse faults of Oligocene–Miocene age. In this area, a temporary seismic network with 16 short-period stations was setup from January to April of 2010, in the context of the MSc thesis of Lira (2010), covering an area of 200 km2 that corresponds with the hydrothermal field of Tinguiririca Volcanic Complex (TVC), Central Chile, Southern Central Andes. Using P- and S- wave arrival times, a 3D seismic velocity tomography was performed. The preliminary locations of 2270 earthquakes have first been determined using an a priori 1D velocity model. Afterwards, a joint inversion of both, the 3D velocity model and final locations have been obtained. High Vp/Vs ratios are interpreted as zones with high hot fluid con tent and high fracturing. Meanwhile, low Vp/Vs anomalies could represent the magmatic reservoir and the con duit network associated to the fluid mobility. Based on structural information and thermal manifestations, these anomalies have been interpreted. In order to visualize the relation between local geology and the velocity model, the volume associated with the magma reservoir and the fluid circulation network has been delimited using an iso-value contour of Vp/Vs equal to 1.70. The most prominent observed feature in the obtained model is a large “V” shaped low-velocity anomaly extending along the entire study region and having the same vergency and ori entation as the existing high-angle inverse faults, which corroborates that El Fierro–El Diablo fault system repre sents the local control for fluid mobility. This geometry coincides with surface hydrothermal manifestations and with available geochemical information of the area, which allowed us to generate a conceptual model of fluid cir culation in the volcanic–hydrothermal system as well as define the location of the magmatic reservoir. © 2015 Elsevier B.V. All rights reservedes
dc.description.urihttps://www-sciencedirect-com.recursosbiblioteca.unab.cl/science/article/pii/S037702731500400X?via%3Dihub
dc.identifier.citationJournal of Volcanology and Geothermal Research. Volume 310, Pages 107 - 117. January 15, 2016es
dc.identifier.doi10.1016/j.jvolgeores.2015.11.018
dc.identifier.issn0377-0273
dc.identifier.urihttps://repositorio.unab.cl/xmlui/handle/ria/54024
dc.language.isoenes
dc.publisherElsevieres
dc.subjectTinguiririca Volcanic Complexes
dc.subjectPassive Seismic Tomographyes
dc.subjectStructural Geologyes
dc.subjectConceptual Modees
dc.titleCharacterization of the hydrothermal system of the Tinguiririca Volcanic Complex, Central Chile, using structural geology and passive seismic tomographyes
dc.typeArtículoes
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