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Ruzié, Lorraine, Moreira, Manuel (2010) Magma degassing process during Plinian eruptions. Journal of Volcanology and Geothermal Research, 192 (3) 142-150 doi:10.1016/j.jvolgeores.2010.02.018

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Reference TypeJournal (article/letter/editorial)
TitleMagma degassing process during Plinian eruptions
JournalJournal of Volcanology and Geothermal Research
AuthorsRuzié, LorraineAuthor
Moreira, ManuelAuthor
Year2010 (May)Volume192
Issue3
PublisherElsevier BV
DOIdoi:10.1016/j.jvolgeores.2010.02.018Search in ResearchGate
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Mindat Ref. ID326573Long-form Identifiermindat:1:5:326573:8
GUID0
Full ReferenceRuzié, Lorraine, Moreira, Manuel (2010) Magma degassing process during Plinian eruptions. Journal of Volcanology and Geothermal Research, 192 (3) 142-150 doi:10.1016/j.jvolgeores.2010.02.018
Plain TextRuzié, Lorraine, Moreira, Manuel (2010) Magma degassing process during Plinian eruptions. Journal of Volcanology and Geothermal Research, 192 (3) 142-150 doi:10.1016/j.jvolgeores.2010.02.018
In(2010, May) Journal of Volcanology and Geothermal Research Vol. 192 (3) Elsevier BV

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Varekamp, Johan C. (1993) Some remarks on volcanic vent evolution during plinian eruptions. Journal of Volcanology and Geothermal Research, 54 (3) 309-318 doi:10.1016/0377-0273(93)90069-4
Chevalier, Laure, Collombet, Marielle, Pinel, Virginie (2017) Temporal evolution of magma flow and degassing conditions during dome growth, insights from 2D numerical modeling. Journal of Volcanology and Geothermal Research, 333. 116-133 doi:10.1016/j.jvolgeores.2017.01.016
Heiken, Grant (1978) Plinian-type eruptions in the medicine lake highland, california, and the nature of the underlying magma. Journal of Volcanology and Geothermal Research, 4 (3) 375-402 doi:10.1016/0377-0273(78)90023-9
Nishimura, Takeshi (2009) Ground deformation caused by magma ascent in an open conduit. Journal of Volcanology and Geothermal Research, 187 (3) 178-192 doi:10.1016/j.jvolgeores.2009.09.001
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Arce, J.L., Gardner, J.E., Macías, J.L. (2013) Pre-eruptive conditions of dacitic magma erupted during the 21.7ka Plinian event at Nevado de Toluca volcano, Central Mexico. Journal of Volcanology and Geothermal Research, 249. 49-65 doi:10.1016/j.jvolgeores.2012.09.012
 
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