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Generation of fine hydromagmatic ash by growth and disintegration of glassy rinds

Journal of Geophysical Research B: Solid Earth

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DOI: 10.1029/2005JB003883

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Abstract

The deposits of mafic hydromagmatic eruptions are more fine grained and variable in vesicularity than dry magmatic deposits. Blocky, equant shapes of many hydromagmatic clasts also contrast with droplet, thread, and bubble wall morphology of dry magmatic fragments. Small (

Additional Publication Details

Publication type:
Article
Publication Subtype:
Journal Article
Title:
Generation of fine hydromagmatic ash by growth and disintegration of glassy rinds
Series title:
Journal of Geophysical Research B: Solid Earth
DOI:
10.1029/2005JB003883
Volume
112
Issue:
2
Year Published:
2007
Language:
English
Larger Work Type:
Article
Larger Work Subtype:
Journal Article