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Microlite orientation in obsidian flow measured by synchrotron X-ray diffraction

Microlite orientation in obsidian flow measured by synchrotron X-ray diffraction

https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_osti_scitechconnect_1461697

Microlite orientation in obsidian flow measured by synchrotron X-ray diffraction

About this item

Full title

Microlite orientation in obsidian flow measured by synchrotron X-ray diffraction

Publisher

Berlin/Heidelberg: Springer Berlin Heidelberg

Journal title

Contributions to mineralogy and petrology, 2018-07, Vol.173 (7), p.1-12, Article 58

Language

English

Formats

Publication information

Publisher

Berlin/Heidelberg: Springer Berlin Heidelberg

More information

Scope and Contents

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...

Alternative Titles

Full title

Microlite orientation in obsidian flow measured by synchrotron X-ray diffraction

Identifiers

Primary Identifiers

Record Identifier

TN_cdi_osti_scitechconnect_1461697

Permalink

https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_osti_scitechconnect_1461697

Other Identifiers

ISSN

0010-7999

E-ISSN

1432-0967

DOI

10.1007/s00410-018-1479-9

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