Pre- and syn-eruptive conditions of a basaltic Plinian eruption at Masaya Volcano, Nicaragua: The Masaya Triple Layer (2.1 ka)

@article{Bamber2020PreAS,
  title={Pre- and syn-eruptive conditions of a basaltic Plinian eruption at Masaya Volcano, Nicaragua: The Masaya Triple Layer (2.1 ka)},
  author={Emily C. Bamber and Fabio Arzilli and Margherita Polacci and Margaret E. Hartley and Jonathan W. Fellowes and Danilo Di Genova and David Chavarr{\'i}a and Jos{\'e} Armando Saballos and Mike R. Burton},
  journal={Journal of Volcanology and Geothermal Research},
  year={2020},
  volume={392},
  pages={106761}
}
Understanding basaltic Plinian activity at Masaya caldera, Nicaragua
<p>Plinian eruptions are the most hazardous yet enigmatic style of volcanism at basaltic systems. The low viscosity of basaltic magma should preclude its fragmentation; however, there are several
Crystallization of peralkaline rhyolitic magmas: pre- and syn-eruptive conditions of the Pantelleria system
Pantelleritic magmas are low-viscosity peralkaline rhyolites which exhibit large differences in eruptive style (explosive to effusive). The processes that promote fragmentation and explosive
Mafic explosive volcanism at Llaima Volcano: 3D x-ray microtomography reconstruction of pyroclasts to constrain shallow conduit processes
Mafic volcanic activity is dominated by effusive to mildly explosive eruptions. Plinian and ignimbrite-forming mafic eruptions, while rare, are also possible; however, the conditions that promote
Magma Pressure-Temperature-Time Paths During Mafic Explosive Eruptions
We have constrained syneruptive pressure-temperature-time (P-T-t) paths of mafic magmas using a combination of short-timescale cooling and decompression chronometers. Recent work has shown that the
High-temperature oxidation of proximal basaltic pyroclasts, 1886 Tarawera, New Zealand
Microlite crystallization in erupting basalt can occur in the conduit, in flight, or in situ after deposition. Distinguishing the products of primary versus secondary (post-fragmentation)
Porosity-permeability relationships in crystal-rich basalts from Plinian eruptions
Magma permeability allows release of exsolved and pressurized volatiles during magma ascent, potentially modulating explosive volcanic eruptions. While porosity-permeability relationships in the
Highly explosive basaltic eruptions driven by CO2 exsolution
TLDR
Evidence is presented for an exsolved CO 2 phase ~15 km beneath Sunset Crater that was the critical driver of rapid magma ascent leading to the explosive eruption of the most explosive basaltic scoria cone eruption yet documented.
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