Volcanic stratigraphy and evidence of magma mixing in the Quaternary Payún Matrú volcano, andean backarc in western Argentina

The Payún Matrú Volcanic Field is located in the Payenia Basaltic Province of the recent back-arc of western Argentina (35°S-38°S). This province is younger than 5 Ma, and most of its volcanic activity took place since 2 Ma. The Payún Matrú Volcanic Field contains two composite volcanoes, Payún Matr...

Descripción completa

Guardado en:
Detalles Bibliográficos
Autores principales: Hernando, Irene Raquel, Llambías, Eduardo Jorge, González, Pablo Diego, Sato, Kei
Formato: Articulo
Lenguaje:Inglés
Publicado: 2012
Materias:
Acceso en línea:http://sedici.unlp.edu.ar/handle/10915/83940
Aporte de:
id I19-R120-10915-83940
record_format dspace
institution Universidad Nacional de La Plata
institution_str I-19
repository_str R-120
collection SEDICI (UNLP)
language Inglés
topic Geología
Alkaline basalts
Back-arc magmatism
Magma mixing
Payún Matrú caldera
spellingShingle Geología
Alkaline basalts
Back-arc magmatism
Magma mixing
Payún Matrú caldera
Hernando, Irene Raquel
Llambías, Eduardo Jorge
González, Pablo Diego
Sato, Kei
Volcanic stratigraphy and evidence of magma mixing in the Quaternary Payún Matrú volcano, andean backarc in western Argentina
topic_facet Geología
Alkaline basalts
Back-arc magmatism
Magma mixing
Payún Matrú caldera
description The Payún Matrú Volcanic Field is located in the Payenia Basaltic Province of the recent back-arc of western Argentina (35°S-38°S). This province is younger than 5 Ma, and most of its volcanic activity took place since 2 Ma. The Payún Matrú Volcanic Field contains two composite volcanoes, Payún Matrú and Payún Liso, and two basaltic fields in an E-W oriented zone, located east and west of the Payún Matrú volcano. Payún Matrú is the largest volcano of this volcanic field, and consists of a shield-shaped edifice with a circular summit caldera of 8 km in diameter. The composition of both composite volcanoes is alkaline and predominantly trachytic, having also minor intermediate lavas. The basaltic fields consist of basalts and trachybasalts, with clinopyroxene and abundant olivine as phenocrysts and also in the groundmass. Textures indicating mixing and mingling processes, such as dusty plagioclases along with clear ones, biotite replaced by anhydrous minerals and two groundmasses with a fluid-fluid relationship, are common in the early pre-caldera stage of Payún Matrú and some post-caldera lavas. The latest post-caldera lavas are trachytic, with clean sanidine phenocrysts without disequilibrium textures. A remarkable characteristic of the Payún Matrú Volcanic Field is the fact that the Payún Matrú caldera is surrounded by basaltic fields at its base, while no basalts were erupted in the caldera region. We propose that the absence of basaltic lavas in the Payún Matrú volcano is due to the presence of a magmatic chamber below it, and that the mafic magmas rising from deeper levels were unable to erupt without interaction with more evolved melts. Intermediate hybrid magmas produced as a consequence of magma mixing and mingling between basaltic and trachytic magmas, are present in the early and mid-history of Payún Matrú volcano. We present here new information about the Quaternary Payún Matrú Volcanic Field derived from field work, petrography, and major element geochemistry and 87 Sr/ 86 Sr isotopic ratios. For the first time a detailed map of the Payún Matrú Volcanic Field and its volcanic stratigraphy, primarily based on field observations, are presented.
format Articulo
Articulo
author Hernando, Irene Raquel
Llambías, Eduardo Jorge
González, Pablo Diego
Sato, Kei
author_facet Hernando, Irene Raquel
Llambías, Eduardo Jorge
González, Pablo Diego
Sato, Kei
author_sort Hernando, Irene Raquel
title Volcanic stratigraphy and evidence of magma mixing in the Quaternary Payún Matrú volcano, andean backarc in western Argentina
title_short Volcanic stratigraphy and evidence of magma mixing in the Quaternary Payún Matrú volcano, andean backarc in western Argentina
title_full Volcanic stratigraphy and evidence of magma mixing in the Quaternary Payún Matrú volcano, andean backarc in western Argentina
title_fullStr Volcanic stratigraphy and evidence of magma mixing in the Quaternary Payún Matrú volcano, andean backarc in western Argentina
title_full_unstemmed Volcanic stratigraphy and evidence of magma mixing in the Quaternary Payún Matrú volcano, andean backarc in western Argentina
title_sort volcanic stratigraphy and evidence of magma mixing in the quaternary payún matrú volcano, andean backarc in western argentina
publishDate 2012
url http://sedici.unlp.edu.ar/handle/10915/83940
work_keys_str_mv AT hernandoireneraquel volcanicstratigraphyandevidenceofmagmamixinginthequaternarypayunmatruvolcanoandeanbackarcinwesternargentina
AT llambiaseduardojorge volcanicstratigraphyandevidenceofmagmamixinginthequaternarypayunmatruvolcanoandeanbackarcinwesternargentina
AT gonzalezpablodiego volcanicstratigraphyandevidenceofmagmamixinginthequaternarypayunmatruvolcanoandeanbackarcinwesternargentina
AT satokei volcanicstratigraphyandevidenceofmagmamixinginthequaternarypayunmatruvolcanoandeanbackarcinwesternargentina
AT hernandoireneraquel estratigrafiavolcanicayevidenciademezclademagmasenelvolcanpayunmatrudelcuaternarioenelretroarcoandinodeargentinaoccidental
AT llambiaseduardojorge estratigrafiavolcanicayevidenciademezclademagmasenelvolcanpayunmatrudelcuaternarioenelretroarcoandinodeargentinaoccidental
AT gonzalezpablodiego estratigrafiavolcanicayevidenciademezclademagmasenelvolcanpayunmatrudelcuaternarioenelretroarcoandinodeargentinaoccidental
AT satokei estratigrafiavolcanicayevidenciademezclademagmasenelvolcanpayunmatrudelcuaternarioenelretroarcoandinodeargentinaoccidental
bdutipo_str Repositorios
_version_ 1764820488206417921