Microlite orientation in obsidian flow measured by synchrotron X-ray diffraction
Author:
Funder
National Science Foundation
U.S. Department of Energy
Publisher
Springer Science and Business Media LLC
Subject
Geochemistry and Petrology,Geophysics
Link
http://link.springer.com/article/10.1007/s00410-018-1479-9/fulltext.html
Reference49 articles.
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2. Befus KS, Zinke RW, Jordan JS, Manga M, Gardner JE (2014) Pre-eruptive storage conditions and eruption dynamics of a small rhyolite dome: Douglas Knob, Yellowstone volcanic field, USA. Bull Volcanol 76(3):1–12. https://doi.org/10.1007/s00445-014-0808-8
3. Befus KS, Manga M, Gardner JE, Williams M (2015) Ascent and emplacement dynamics of obsidian lavas inferred from microlite textures. Bull Volcanol 77(10):88. https://doi.org/10.1007/s00445-015-0971-6
4. Buisson C, Merle O (2002) Experiments on internal strain in lava dome cross sections. Bull Volcanol 64(6):363–371. https://doi.org/10.1007/s00445-002-0213-6
5. Castro J, Cashman KV (1999) Constraints on rheology of obsidian lavas based on mesoscopic folds. J Struct Geol 21(7):807–819. https://doi.org/10.1016/S0191-8141(99)00070-X
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