2021
DOI: 10.1007/s00445-020-01426-z
|View full text |Cite
|
Sign up to set email alerts
|

Mechanism of the historical and the ongoing Vulcanian eruptions of Ebeko volcano, Northern Kuriles

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
2
1

Citation Types

0
3
0
2

Year Published

2022
2022
2024
2024

Publication Types

Select...
6
1
1

Relationship

0
8

Authors

Journals

citations
Cited by 16 publications
(5 citation statements)
references
References 45 publications
0
3
0
2
Order By: Relevance
“…The high activity of northern volcanoes Sheveluch, Klyuchevskoy, Bezymyanny, Plosky, and Tolbachik was manifested in the records at seismic stations KIR, KLY, KOZ, and at TUMD station during the Kizimen volcano activation in 2011-2013. Weak signals from gas-ash emissions appeared in the records at SKR station during the Ebeko volcano eruption in 2016-2021 [32][33][34]. Brief episodes of increased activity from the Avachinsky volcano appeared in records at AVH station.…”
Section: Volcanic Stationsmentioning
confidence: 99%
“…The high activity of northern volcanoes Sheveluch, Klyuchevskoy, Bezymyanny, Plosky, and Tolbachik was manifested in the records at seismic stations KIR, KLY, KOZ, and at TUMD station during the Kizimen volcano activation in 2011-2013. Weak signals from gas-ash emissions appeared in the records at SKR station during the Ebeko volcano eruption in 2016-2021 [32][33][34]. Brief episodes of increased activity from the Avachinsky volcano appeared in records at AVH station.…”
Section: Volcanic Stationsmentioning
confidence: 99%
“…Cpx is a stable phase over a very wide range of pressures, temperatures, melt compositions and oxygen fugacities (e.g., Costa, 2004;Nandedkar et al, 2014;Ulmer et al, 2018), meaning Cpx-based thermobarometry has broad utility and has been applied in a wide variety of tectonic settings. In this contribution we specifically focus on the use of Cpx-based thermobarometer to investigate storage conditions in magmas erupted in subduction zones (see Table . 1 for studies performing such calculations; Auer et al, 2013;Belousov et al, 2021;Cassidy et al, 2015;Caulfield et al, 2012;Cigolini et al, 2018;Dahren et al, 2012;Deegan et al, 2016;Freundt and Kutterolf, 2019;Geiger et al, 2018;Hollyday et al, 2020;Jeffery et al, 2013;Lai et al, 2018;Lormand et al, 2021;Moussallam et al, 2021Moussallam et al, , 2019Namur et al, 2020;Preece et al, 2014;Romero et al, 2022;Ruth and Costa, 2021;Sas et al, 2017;Scruggs and Putirka, 2018;Sheehan and Barclay, 2016).…”
Section: Introductionmentioning
confidence: 99%
“…In contrast, volcanoes prone to low- to moderate-intensity explosive activity, such as phreatic, Surtseyan, Strombolian, violent Strombolian, and Vulcanian eruptions, are characterized by the repetitive emplacement of fine-grained and moderately dispersed tephra beds in the down-wind sectors from the source vent, resulting in more complex tephro-stratigraphic studies (Walker 1973 ; Newhall and Self 1982 ; Arrighi et al 2001 ; Yasui and Koyaguchi 2004 ; de Vita et al 2010 ; Pistolesi et al 2016 , 2017 ; Bernard and Bouvet de Maisonneuve 2020 ; Belousov et al 2021 ; Drymoni et al 2023 ; Vallejo et al 2024 ).…”
Section: Introductionmentioning
confidence: 99%