The role of magma mixing and mafic recharge in the evolution of a back-arc quaternary caldera: The case of Payún Matrú, Western Argentina.

HERNANDO IRENE; PETRINOVIC IVÁN; LLAMBÍAS EDUARDO; D'ELÍA LEANDRO; GONZÁLEZ PABLO DIEGO; ARAGÓN, EUGENIO

JOURNAL OF VOLCANOLOGY AND GEOTHERMAL RESEARCH

ELSEVIER SCIENCE BV

Lugar: Amsterdam; Año: 2016 vol. 311 p. 150 - 169

0377-0273

The Quaternary Payun Matru volcano is a long-lived edifice that developed a summit caldera 8 km wide, with abundant pre- and post-caldera volcanic activity. It is the main volcano of the Payun Matru Volcanic Field, which is located in the back-arc Payenia Basaltic Province, at mid-western Argentina. The composition of Payun Matru is mainly trachytic, with lesser amounts of trachyandesitic and basaltic trachyandesitic lavas. The Payun Matru Volcanic Field includes also the Payun Liso stratovolcano and more than 200 monogenetic basaltic cones and associated lava flows that are located east and west of the caldera. The aim of this work is to show the Payun Matru evolution based on the mineralogical and textural characterization and to make inferences on the trigger mechanism for the explosive eruption which leads to the caldera formation. Some intermediate lavas and trachytes include phenocrysts with contrasting textures and composition, such as inverse zoning in plagioclase and clinopyroxenes, sieved plagioclases with a more calcic rim and calcic plagioclases with a more sodic rim, indicating that they could not have formed together and suggesting magma mixing processes. In addition, a few lavas show mafic enclaves or texturally different groundmasses with fluidal contacts, indicating mingling between two magmas. These lavas are found in the pre-caldera stage and the early post-caldera stage of Payun Matru. The trachytic pyroclastic deposits related to the caldera collapse do not exhibit evidence of hybridization, although they present a minor proportion of dissolved feldspars and biotite replaced by anhydrous minerals, suggesting that a restricted zone of the chamber was reheated. This may be explained by a mafic recharge event where part of the host trachytic magma was heated, but without a complete homogenization between the host and recharging magmas. These features, in addition to the abundant basaltic volcanism east and west of the caldera, suggest that the trigger mechanism for the explosive eruption was the injection of basaltic magma into the trachytic chamber of Payun Matru.