Vulcanismo cuaternario de la Isla Decepción (Antártida): Una signatura relacionada con la subducción de la Fosa de las Shetland del Sur en el dominio de tras-arco de la Cuenca de Bransfield

Galé, C. (Universidad de Zaragoza) ; Ubide, T. ; Lago, M. (Universidad de Zaragoza) ; Gil-Imaz, A. (Universidad de Zaragoza) ; Gil-Peña, I. ; Galindo-Zaldívar, J. ; Rey, J. ; Maestro, A. ; López-Martínez, J.

Resumen: Deception Island shows a volcanism related to the Phoenix Plate subduction and roll-back under South Shet- land Block in the present times. The development of the island is related to the evolution and collapse of a volcanic caldera, and this study is focused on the petrology, mineralogy and geochemistry of the post-caldera rocks. We have made a study of the lava flows, dikes and the youngest historic eruption in 1970. These rocks range from dacite to rhyolite and have a microporphyritic texture with olivine and minor clinopyroxene. A pre-caldera basaltic andesite has also been studied. It has a microporphyritic texture with clinopyroxene.The intermediate and acid compositions alternating in the volcanostratigraphic sequence suggest either mafic recharge events or melt extraction from different levels in the deep magmatic system. All the studied compo- sitions share a subduction-related signature similar to other magmatics from the Bransfield Basin. However, compositional differences between pre-caldera and post-caldera rocks indicate a different magma source and depth of crystallisation. According to the geothermobarometric calculations the pre-caldera magmas started to crystallise at deeper levels (13.5–15 km) than the post-caldera magmas (6.2–7.8 km). Specifically, the post- caldera magmas indicate a smaller influence of the subducting slab in the southwestern part of the Bransfield Basin in respect to the available data from other sectors as well as the involvement of crustal contamination in the genesis of the magmas.

Idioma: Español

Año: 2013

Publicado en: Boletin Geologico y Minero 125, 1 (2013), 31-52
ISSN: 0366-0176

Originalmente disponible en: Texto completo de la revista

Financiación: info:eu-repo/grantAgreement/ES/MINECO/CTM2011-13902-E
Financiación: info:eu-repo/grantAgreement/ES/MINECO/CTM2011-26372
Financiación: info:eu-repo/grantAgreement/ES/MINECO/CTM2011-30241-C02-02

Tipo y forma: Artículo (Versión definitiva)

Área (Departamento): Geodinámica Interna (Departamento de Ciencias de la Tierra)
Área (Departamento): Petrología y Geoquímica (Departamento de Ciencias de la Tierra)