Ascent and emplacement dynamics of obsidian lavas inferred from microlite textures
Ascent and emplacement dynamics of obsidian lavas inferred from microlite textures
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Berlin/Heidelberg: Springer Berlin Heidelberg
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Language
English
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Berlin/Heidelberg: Springer Berlin Heidelberg
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Contents
To assess the eruption and emplacement of volumetrically diverse rhyolite lavas, we measured microlite number densities and orientations from samples collected from nine lavas in Yellowstone Caldera and two from Mono Craters, USA. Microlite populations are composed of Fe-Ti oxides ± alkali feldspar ± clinopyroxene. Number densities range from 10
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Full title
Ascent and emplacement dynamics of obsidian lavas inferred from microlite textures
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TN_cdi_osti_scitechconnect_1480692
Permalink
https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_osti_scitechconnect_1480692
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ISSN
0258-8900
E-ISSN
1432-0819
DOI
10.1007/s00445-015-0971-6
