Conduit stability effects on intensity and steadiness of explosive eruptions
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[1] P. Landi,et al. Correction to: CrystalMom: a new model for the evolution of crystal size distributions in magmas with the quadrature-based method of moments , 2018, Contributions to Mineralogy and Petrology.
[2] C. Simone,et al. CrystalMom: a new model for the evolution of crystal size distributions in magmas with the quadrature-based method of moments , 2017, Contributions to Mineralogy and Petrology.
[3] A. Neri,et al. Stability of volcanic conduits during explosive eruptions , 2017 .
[4] Augusto Neri,et al. Uncertainty quantification and sensitivity analysis of volcanic columns models: results from the integral model PLUME-MoM , 2016 .
[5] Martin Nayembil,et al. Global database on large magnitude explosive volcanic eruptions (LaMEVE) , 2012, Journal of Applied Volcanology.
[6] B. Tikoff,et al. Transtensional deformation and structural control of contiguous but independent magmatic systems: Mono-Inyo Craters, Mammoth Mountain, and Long Valley Caldera, California , 2012 .
[7] R. Cioni,et al. The 512 AD eruption of Vesuvius: complex dynamics of a small scale subplinian event , 2011 .
[8] M. Bursik,et al. Subplinian fall deposits of Inyo Craters, CA , 2010 .
[9] B. Voight,et al. Effects of conduit geometry on magma ascent dynamics in dome-forming eruptions , 2008 .
[10] Robert W. Zimmerman,et al. Stability analysis of vertical boreholes using the Mogi–Coulomb failure criterion , 2006 .
[11] R. Sulpizio,et al. A complex, Subplinian-type eruption from low-viscosity, phonolitic to tephri-phonolitic magma: the AD 472 (Pollena) eruption of Somma-Vesuvius, Italy , 2005 .
[12] G. Walker,et al. Variability of plinian fall deposits: examples from Okataina Volcanic Centre, New Zealand , 2001 .
[13] G. Walker,et al. The intensity and magnitude of the Mangaone subgroup plinian eruptions from Okataina Volcanic Centre, New Zealand , 2001 .
[14] G. Walker,et al. Stratigraphy and dispersal of the Mangaone Subgroup pyroclastic deposits, Okataina Volcanic Centre, New Zealand , 2000 .
[15] Paolo Papale,et al. The role of magma composition and water content in explosive eruptions: 1. Conduit ascent dynamics , 1998 .
[16] P. Cole,et al. An historic subplinian/phreatomagmatic eruption: the 1630 AD eruption of Furnas volcano, Sa˜o Miguel, Azores , 1995 .
[17] M. Bursik. Subplinian eruption mechanisms inferred from volatile and clast dispersal data , 1993 .
[18] F. Dobran. Nonequilibrium flow in volcanic conduits and application to the eruptions of Mt. St. Helens on May 18, 1980, and Vesuvius in AD 79 , 1992 .
[19] J. Fink,et al. The mechanism of intrusion of the Inyo Dike, Long Valley Caldera, California , 1988 .
[20] K. Sieh,et al. Most recent eruption of the Mono Craters, eastern central California , 1986 .
[21] S. Malone,et al. Magma supply, magma discharge and readjustment of the feeding system of mount St. Helens during 1980 , 1985 .
[22] G. Walker. The Taupo pumice: Product of the most powerful known (ultraplinian) eruption? , 1980 .
[23] Andrea Rowland-Smith. The 1630 AD eruption of Furnas Volcano, São Miguel, Azores (Portugal): chemical variations and magmatic processes , 2007 .
[24] A. Neri,et al. Erosion processes in volcanic conduits and application to the AD 79 eruption of Vesuvius , 1994 .
[25] W. Hildreth,et al. Volcán Quizapu, Chilean Andes , 1992 .
[26] C. Miller,et al. Holocene eruptions at the Inyo volcanic chain, California: Implications for possible eruptions in Long Valley caldera , 1985 .