Hostname: page-component-78c5997874-fbnjt Total loading time: 0 Render date: 2024-11-13T11:31:11.611Z Has data issue: false hasContentIssue false
  • English
  • Français

Fragmentation, nucleation and migration of crystals and bubbles in the Bishop Tuff rhyolitic magma

Published online by Cambridge University Press:  26 July 2007

Guilherme A. R. Gualda ,
David L. Cook ,
Rahul Chopra ,
Liping Qin ,
Alfred T. Anderson Jr  and
Mark Rivers
Guilherme A. R. Gualda
Affiliation:
Department of the Geophysical Sciences, The University of Chicago, 5734 S. Ellis Avenue, Chicago, IL 60637, USA.
David L. Cook
Affiliation:
Department of the Geophysical Sciences, The University of Chicago, 5734 S. Ellis Avenue, Chicago, IL 60637, USA.
Rahul Chopra
Affiliation:
Department of the Geophysical Sciences, The University of Chicago, 5734 S. Ellis Avenue, Chicago, IL 60637, USA.
Liping Qin
Affiliation:
Department of the Geophysical Sciences, The University of Chicago, 5734 S. Ellis Avenue, Chicago, IL 60637, USA.
Alfred T. Anderson Jr
Affiliation:
Department of the Geophysical Sciences, The University of Chicago, 5734 S. Ellis Avenue, Chicago, IL 60637, USA.
Mark Rivers
Affiliation:
Consortium for Advanced Radiation Sources, The University of Chicago, Building 434A, 9700 South Cass, Argonne, IL 60439, USA.
Get access Rights & Permissions [Opens in a new window]

Abstract

The Bishop Tuff (USA) is a large-volume, high-silica pyroclastic rhyolite. Five pumice clasts from three early stratigraphic units were studied. Size distributions were obtained using three approaches: (1) crushing, sieving and winnowing (reliable for crystals >100 μm); (2) microscopy of ∼1 mm3 fragments (preferable for crystals <100 μm); and (3) computerised X-ray microtomography of ∼1 cm3 pumice pieces.

Phenocryst fragments coated with glass are common, and the size distributions for all crystals are concave-upward, indicating that crystal fragmentation is an important magmatic process.

Three groups are recognised, characterised by: (1) high-density (0·759–0·902 g cm−3), high-crystal content (14·4–15·3 wt.%) and abundant large crystals (>800 μm); concave-downward size distributions for whole crystals indicate late-stage growth with limited nucleation, compatible with the slow cooling of a large, gas-saturated, stably stratified magma body; (2) low-density (0·499 g cm −3), low-crystal content (6·63 wt.%) and few large crystals; the approximately linear size distribution reveals that nucleation was locally important, perhaps close to the walls; and (3) intermediate characteristics in all respects.

The volumetric fraction of bubbles inversely correlates with the number of large crystals. This is incompatible with isobaric closed-system crystallisation, but can be explained by sinking of large crystals and rise of bubbles in the magma

Keywords

Crystal ContentCrystal Size DistributionMagmatic ProcessesPumice DensityRhyolites
Type
Research Article
Information
Earth and Environmental Science Transactions of The Royal Society of Edinburgh , Volume 95 , Issue 1-2 , March 2004 , pp. 375 - 390
Copyright
Copyright © Royal Society of Edinburgh 2004

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)