Volume 4 Quaternary Chapter 4 Neogene https://doi.org/10.32685/pub.esp.38.2019.04 Paipa Geothermal System, Boyacá: Review Published online 20 May 2020 of Exploration Studies and Conceptual Model Paleogene Claudia María ALFARO–VALERO1* , Jesús Bernardo RUEDA–GUTIÉRREZ2 , 3 4 Jhon Camilo MATIZ–LEÓN , Miguel Angel BELTRÁN–LUQUE , 1
[email protected] 5 6 Gilbert Fabián RODRÍGUEZ–RODRÍGUEZ , Gina Z. RODRÍGUEZ–OSPINA , Servicio Geológico Colombiano 7 8 Dirección de Geociencias Básicas Carlos Eduardo GONZÁLEZ–IDÁRRAGA , and Jaison Elías MALO–LÁZARO Diagonal 53 n.° 34–53 Cretaceous Bogotá, Colombia Abstract The Paipa geothermal system is located at 2525 masl in a terrain tilted from 2
[email protected] Servicio Geológico Colombiano south to north towards the Chicamocha River, where the geology is dominated by Dirección de Geociencias Básicas sedimentary rocks intruded by felsic magmas. The Miocene and Pleistocene volcanic Diagonal 53 n.° 34–53 Bogotá, Colombia activity produced pyroclastic deposits and dome complexes. A deep saline sodium Jurassic 3
[email protected] sulfate water, presumably originating from the infiltration of meteoric water followed Servicio Geológico Colombiano Dirección de Geociencias Básicas by dissolution of an evaporite, mixes with geothermal fluid. This process masks the Diagonal 53 n.° 34–53 chemical and isotopic composition of the geothermal component of fluid discharge in Bogotá, Colombia 4
[email protected] hot springs, the temperatures of which reach 76 °C. Organic and magmatic/mantle con- Servicio Geológico Colombiano Triassic tributions also affect the composition of the gas phase discharges. High concentrations Dirección de Geociencias Básicas Diagonal 53 n.° 34–53 of radioactive elements are found in the area, mainly in El Durazno Intrusive, a highly Bogotá, Colombia altered intrusion located to the west.