Evolution of Irruputuncu volcano,Central Andes,northern Chile |
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| Institution: | 1. Departamento de Geología, Facultad de Ciencias Físicas y Matemáticas, Universidad de Chile, Plaza Ercilla 803, Santiago, Chile;2. Centro de Excelencia en Geotermia de los Andes (CEGA), Facultad de Ciencias Físicas y Matemáticas, Universidad de Chile, Plaza Ercilla 803, Santiago, Chile;3. Colegio de Geografía, Facultad de Filosofía y Letras, SUAyED, UNAM, Ciudad Universitaria, 04510 Ciudad de Mexico, Mexico;4. Facultad de Ingeniería, Arquitectura y Diseño, Universidad San Sebastián, Bellavista 7, Recoleta, Santiago 8420524, Chile;5. Department of Geological Sciences, University of Cape Town, Rondebosch 7700, South Africa;6. School of Environment, The University of Queensland, Brisbane, 4102 QLD, Australia;1. Leibniz Universität Hannover, Institut of Mineralogy, Callinstr. 3, 30167 Hannover, Germany;2. Geowissenschaftliches Zentrum Göttingen, Abteilung Geochemie, Goldschmidtstr. 1, 37077 Göttingen, Germany;3. Technische Universität Berlin, Fachgebiet Mineralogie, Ackerstr. 76, 13355 Berlin, Germany;1. Departamento de Geología, Universidad de Chile, Plaza Ercilla 803, Santiago, Chile;2. Centro de Excelencia en Geotermia de los Andes (CEGA), Universidad de Chile, Plaza Ercilla 803, 8370450, Santiago, Chile;3. Dipartimento di Scienze della Terra, Via G. La Pira 4, 50121 Firenze, Italy;4. CNR-IGG Istituto di Geoscienze e Georisorse, Via G. La Pira 4, 50121, Firenze, Italy;5. Servicio Nacional de Geología y Minería, Av. Santa María Chaina 0104, Santiago, Chile;6. Istituto Nazionale Geofisica e Vulcanologia INGV, Sez. di Palermo, Via U. La Malfa 153, 90145 Palermo, Italy |
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| Abstract: | The Irruputuncu is an active volcano located in northern Chile within the Central Andean Volcanic Zone (CAVZ) and that has produced andesitic to trachy-andesitic magmas over the last ～258 ± 49 ka. We report petrographical and geochemical data, new geochronological ages and for the first time a detailed geological map representing the eruptive products generated by the Irruputuncu volcano. The detailed study on the volcanic products allows us to establish a temporal evolution of the edifice. We propose that the Irruputuncu volcanic history can be divided in two stages, both dominated by effusive activity: Irruputuncu I and II. The oldest identified products that mark the beginning of Irruputuncu I are small-volume pyroclastic flow deposits generated during an explosive phase that may have been triggered by magma injection as suggested by mingling features in the clasts. This event was followed by generation of large lava flows and the edifice grew until destabilization of its SW flank through the generation of a debris avalanche, which ended Irruputuncu I. New effusive activity generated lavas flows to the NW at the beginning of Irruputuncu II. In the meantime, lava domes that grew in the summit were destabilized, as shown by two well-preserved block-and-ash flow deposits. The first phase of dome collapse, in particular, generated highly mobile pyroclastic flows that propagated up to ～8 km from their source on gentle slopes as low as 11° in distal areas. The actual activity is characterized by deposition of sulfur and permanent gas emissions, producing a gas plume that reaches 200 m above the crater. The maximum volume of this volcanic system is of ～4 km3, being one of the smallest active volcano of Central Andes. |
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| Keywords: | Irruputuncu volcano Central Andes Debris avalanche Block and ash flow Lava flow |
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