Causes of fragmented crystals in ignimbrites: a case study of the Cardones ignimbrite, Northern Chile
Author:
Funder
BHP Billiton
AXA Research Fund
Publisher
Springer Science and Business Media LLC
Subject
Geochemistry and Petrology
Link
http://link.springer.com/article/10.1007/s00445-018-1196-2/fulltext.html
Reference64 articles.
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2. Allen S, McPhie J (2003) Phenocryst fragments in rhyolitic lavas and lava domes. J Volcanol Geotherm Res 126(3):263–283. https://doi.org/10.1016/S0377-0273(03)00151-3
3. Bachmann O, Dungan M, Lipman P (2000) Voluminous lava-like precursor to a major ash-flow tuff: low-column pyroclastic eruption of the Pagosa Peak Dacite, San Juan volcanic field, Colorado. J Volcanol Geotherm Res 98(1):153–171
4. Best MG, Christiansen EH (1997) Origin of broken phenocrysts in ash-flow tuffs. Geol Soc Am Bull 109(1):63–73. https://doi.org/10.1130/0016-7606(1997)109<0063:OOBPIA>2.3.CO;2
5. Bindeman IN (2005) Fragmentation phenomena in populations of magmatic crystals. Am Mineral 90(11–12):1801–1815. https://doi.org/10.2138/am.2005.1645
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