Tracking bubble evolution inside a silicic dike

Antonio M. Álvarez-Valero, Satoshi Okumura, Fabio Arzilli, Javier Borrajo, Clemente Recio, Masao Ban, Juan C. Gonzalo, José M. Benítez, Madison Douglas, Osamu Sasaki, Piedad Franco, Juan Gómez-Barreiro, Asunción Carnicero

Research output: Contribution to journalArticlepeer-review

168 Downloads (Pure)

Abstract

Pressure estimates from rapidly erupted crustal xenoliths constrain the depth of intrusion of the silicic lavas hosting them. This represents an opportunity for tracking magmatic bubble's evolution and quantifying the variation in bubble volume during rapid magma ascent through a volcanic dike just prior to eruption. The petrology, stable-isotope geochemistry and X-ray micro-tomography of dacites containing crustal xenoliths, erupted from a Neogene volcano in SE Spain, showed an increase in porosity from ~ 1.7 to 6.4% from ~ 19 to 13 km depth, at nearly constant groundmass and crystal volumes. This result provides additional constraints for experimental and numerical simulations of subvolcanic magma-crust degassing processes in silicic systems, and may allow the characterization of volcanic eruptive styles based on volatile content.

Original languageEnglish
Pages (from-to)668-676
Number of pages9
JournalLithos
Volume262
Early online date16 Aug 2016
DOIs
Publication statusPublished - 1 Oct 2016

Keywords

  • Conduit depths
  • Crustal xenoliths
  • Dacite
  • Stable isotopes
  • Volcanic bubbles
  • X-ray micro-tomography

Fingerprint

Dive into the research topics of 'Tracking bubble evolution inside a silicic dike'. Together they form a unique fingerprint.

Cite this