Effects of structural zonation on fluids circulation of the copahue geothermal system

YAGUPSKY, DANIEL L.; BARCELONA, HERNÁN P.; VIGIDE, NICOLÁS C.; LOSSADA, ANA C.

JOURNAL OF SOUTH AMERICAN EARTH SCIENCES

PERGAMON-ELSEVIER SCIENCE LTD

Año: 2023

0895-9811

The volcano-hosted geothermal system of Copahue is one of the most promising resources of renewable energy inArgentina. The associated geothermal field is bounded by a set of N60◦ trending normal faults to the north and byWNW-ESE trending faults to the south. This paper aims to review this first-order distribution of the structures,using previously published b-value data, and to explore the relationship between the local stress field, the superficialstructural setting, the magmatic source, and the geothermal fluid flow paths related to the volcaniccomplex. The 2D dilation tendencies of the geomorphic lineaments is calculated, defining a structural domainwith dilatant lineaments that agrees well with high b-values observed at shallow depths(2 km below the surface),and with the known extension of the geothermal field. A rough spatial correspondence is also observed betweendomains of unfavorable oriented to dilate lineaments and shallow low b-value areas, suggesting that these discontinuitiesinhibit the horizontal motion of fluids at the same structural level, and constraining the reservoirboth to the northwest and to the southeast. b-value data unravels the potential magmatic plumbing system atdepth, highlighting a major NW-elongated high b-value body centered at 5 km below surface, from Chancho-c´ohill towards the south of Maquinas fumaroles. It is coincident at surface with a high density of lineament intersectionsdomain, which creates in depth an intense structural damage zone that may facilitate the ascent ofmagmatic fluids. The NW anomaly can be extrapolated to the western margin of the Caviahue lake, agreeing withthe occurrence of volcano-tectonic seismic events and elevated heat flows reported in this area, and thereforesuggesting the presence of the geothermal reservoir at depth. Vertical appendices branching from the b-valueanomaly reach up to 3 km below Termas and Maquinitas fumaroles, outlining the possible bottom of thegeothermal reservoir. The shallower one is interpreted as a blob of magma injected below the Copahue Villagefault system, providing the main heat source. These findings contribute to the current understanding of thegeothermal reservoir, its depth coverage and upflow zones, providing insights for future geophysical explorationstages.