Growth and collapse of the 2018–2019 lava dome of Merapi volcano
Author:
Funder
Agence nationale de la recherche
LabEx ClerVolc
Publisher
Springer Science and Business Media LLC
Subject
Geochemistry and Petrology
Link
http://link.springer.com/content/pdf/10.1007/s00445-020-01428-x.pdf
Reference35 articles.
1. Abdurachman EK, Bourdier JL, Voight B (2000) Nuées ardentes of 22 November 1994 at Merapi volcano, Java, Indonesia. J Volcanol Geotherm Res 100(1):345–361. https://doi.org/10.1016/S0377-0273(00)00144-X
2. Blake S, Bruno BC (2000) Modelling the emplacement of compound lava flows. Earth Planet Sci Lett 184:181–197. https://doi.org/10.1016/S0012-821X(00)00278-8
3. Brodscholl A, Kirbani SB, Voight B (2000) Sequential dome-collapse nuées ardentes analyzed from broadband seismic data, Merapi Volcano, Indonesia. J Volcanol Geotherm Res 100(2000):363–369. https://doi.org/10.1016/S0377-0273(00)00145-1
4. Carn SA, Watts RB, Thompson G, Norton GE (2004) Anatomy of a lava dome collapse: the 20 March 2000 event at Soufriere Hills Volcano, Montserrat. J Volcanol Geotherm Res 100:241–264. https://doi.org/10.1016/S0377-0273(03)00364-0
5. Charbonnier SJ, Gertisser R (2008) Field observations and surface characteristics of pristine block-and-ash flow deposits from the 2006 eruption of Merapi Volcano, Java, Indonesia. J Volcanol Geotherm Res 177(4):971–982. https://doi.org/10.1016/j.jvolgeores.2008.07.008
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