Litofacies y mineralogía de los depósitos de sínter de la zona geotérmica de San Agustín del Maíz, Michoacán, México

Abstract

In the active San Agustín del Maíz geothermal zone (Michoacán), we identified silica-sinter deposits co-existing with hot springs. Considering the deposition mode, these deposits are separated into fracture-banded and bedded deposits. The first ones are associated with deposition on the channels from the fluids rising to the surface, while the second ones are formed from the geothermal fluids that reached the surface. The bedded deposits showed different types of lithofacies grouped in a range with two endmembers: on the one hand, a pure silica-sinter deposit characterized by high density, glassy aspect and being consolidated. On the other hand, a silty-sandy deposit, that easily disaggregate, presenting impression of plants and lithics. The vitreous deposit is considered geyserite, formed from fluids with temperatures superior to 70 °C, while the silty-sandy deposits are formed from fluids with temperatures below 70 °C and, in some cases, far away from the water source. The geyserite deposits are mineralogically composed only by opal (C and CT), while the silty-sandy deposits are formed by opal in association with other mineralogical phases (linked to sediments). Consequently, we recognized that the lithofacies and the mineralogy of the silica-sinter deposits give information of the temperatures and deposition rates of the parental fluids. This information could be very useful in order to identify setting where existed grater geothermal up flow and temperature (e.g. geiserite Litofacies y mineralogía de los depósitos de sínter de la zona geotérmica de San Agustín del Maíz, Michoacán, México Emmanuel Olvera-García1, 2,*, Víctor Hugo Garduño-Monroy1, Mikhail Ostrooumov1, Gerardo Bermejo-Santoyo1, Jorge Alejandro Guevara-Alday3, Andrea Brogi2 y Domenico Liotta2 1 Universidad Michoacana de San Nicolás de Hidalgo, Instituto de Investigación en Ciencias de la Tierra, Morelia, Michoacán, México. 2 Università degli Studi di Bari, Dipartimento di Scienze della Terra e Geoambientali, Bari, Italia. 3 University of Quebec in Montreal, Department of Earth and Atmospheric Science, Montreal, Canada. * emmanuelog_08@outlook.com REVISTA MEXICANA DE CIENCIAS GEOLÓGICAS v. 37, núm. 3, 2020, p. 212-223 I: htt ://dx.doi.org/10.22201/cgeo.20072902e.2020.3.1585 213 Sínter de la zona geotérmica de San Agustín del Maíz, Michoacán, México RMCG | v. 37 | núm. 3 | www.rmcg.unam.mx | DOI: http://dx.doi.org/10.22201/cgeo.20072902e.2020.3.1585 a) b) Depósitos lacustres y aluviales Mio-Holocénicos Volcanes y productos volcánicos (de ácidos a básicos) del Mioceno tardío al Holoceno Lavas (andesíticas y basálticas) y depósitos ignimbríticos del Mioceno medio y tardío Fallas de normal a oblicua izquierda Falla de lateral a oblicua 3.