Rodriguez I., Roche Olivier, Moune S., Aguilera F., Campos E., Pizarro M. (2015). Evolution of Irruputuncu volcano, Central Andes, northern Chile. Journal of South American Earth Sciences, 63, p. 385-399. ISSN 0895-9811.
Titre du document
Evolution of Irruputuncu volcano, Central Andes, northern Chile
Rodriguez I., Roche Olivier, Moune S., Aguilera F., Campos E., Pizarro M.
Source
Journal of South American Earth Sciences, 2015,
63, p. 385-399 ISSN 0895-9811
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 similar to 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 similar to 8 km from their source on gentle slopes as low as 11 degrees 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 similar to 4 km(3), being one of the smallest active volcano of Central Andes.
