Microlite orientation in obsidian flow measured by synchrotron X-ray diffraction
Microlite orientation in obsidian flow measured by synchrotron X-ray diffraction
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Publisher
United States: Springer
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Language
English
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Publisher
United States: Springer
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Contents
Clinopyroxene and plagioclase (andesine) microlites in an obsidian flow from Glass Mountain (NE California, USA) display strong alignment. Synchrotron X-ray diffraction, coupled with Rietveld analysis, was used to quantify crystallographic-preferred orientation (CPO). Clinopyroxene, with a rod-shaped morphology, shows a strong alignment of [001] in...
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Full title
Microlite orientation in obsidian flow measured by synchrotron X-ray diffraction
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TN_cdi_osti_scitechconnect_1561893
Permalink
https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_osti_scitechconnect_1561893
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ISSN
0010-7999
E-ISSN
1432-0967
DOI
10.1007/s00410-018-1479-9
