Silicic conduits as supersized tuffisites: Clastogenic influences on shifting eruption styles at Cordón Caulle volcano (Chile)
Author:
Publisher
Springer Science and Business Media LLC
Subject
Geochemistry and Petrology
Link
http://link.springer.com/content/pdf/10.1007/s00445-020-01432-1.pdf
Reference83 articles.
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2. Alidibirov M, Dingwell DB (2000) Three fragmentation mechanisms for highly viscous magma under rapid decompression. J Volcanol Geotherm Res 100:413–421
3. Alloway BV, Pearce NJG, Villarosa G, Outes V, Moreno PI (2015) Multiple melt bodies fed the AD 2011 eruption of Puyehue-Cordón Caulle, Chile. Sci Rep 5:17589. https://doi.org/10.1038/srep17589
4. Browning J, Tuffen H, James MR, Owen J, Castro JM, Halliwell S, Wehbe K (2020) Post-fragmentation vesiculation timescales in hydrous rhyolitic bombs from Chaitén volcano. J S Am Earth Sci 104:102807. https://doi.org/10.1016/j.jsames.2020.102807
5. Cabrera A, Weinberg RF, Wright HMN, Zlotnik S, Cas RAF (2011) Melt fracturing and healing: a mechanism for degassing of silicic obsidian. Geology 39:67–70. https://doi.org/10.1130/G31355.1
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