Feeding of a magma chamber by an ascending magma bubble [PDF]
Geophysical Journal International, 2021 SUMMARY There is evidence that magma chambers are not fed by a continuous flow, but in the form of discrete magma batches. The possibility is considered that the chamber is fed by a magma bubble ascending through the region underneath, driven by buoyancy force.
Dragoni M.
openaire +2 more sources
Volatile resorption expedites eruption onset in large silicic systems [PDF]
Nature CommunicationsSilicic caldera-forming eruptions are among the most hazardous natural phenomena on Earth, yet their triggering mechanisms remain poorly understood. While volatile exsolution is widely recognized as a potential eruption driver in large silicic systems ...
Franziska Keller +3 more
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Geophysical Research Letters, 2016 The Wudalianchi Volcano Field (WDF) is a typical intraplate volcano in northeast China with generation mechanism not yet well understood. As its last eruption was around 300 years ago, the present risk for volcano eruption is of particular public ...
Zhiwei Li +6 more
doaj +2 more sources
, 2019 Newsletter sent to members of the Huntsville Chamber of ...
Huntsville Chamber of Commerce
core +14 more sources
Repressurization following eruption from a magma chamber with a viscoelastic aureole
Journal of Geophysical Research: Solid Earth, 2016 Paul Segall
exaly +2 more sources
Micro-analytical Perspectives on the Bishop Tuff and its Magma Chamber [PDF]
, 2015 New in situ major and trace element analytical data are presented for crystals (sanidine, plagioclase, biotite, orthopyroxene, clinopyroxene) and matrix glasses from juvenile materials representing the full Bishop Tuff sequence from the earliest fall ...
K. Chamberlain +3 more
semanticscholar +2 more sources
Radiometric Constraints on the Timing, Tempo, and Effects of Large Igneous Province Emplacement
Geophysical Monograph Series, Page 27-82., 2021 Exploring the links between Large Igneous Provinces and dramatic environmental impact
An emerging consensus suggests that Large Igneous Provinces (LIPs) and Silicic LIPs (SLIPs) are a significant driver of dramatic global environmental and biological changes, including mass extinctions.
Jennifer Kasbohm +2 more
wiley +2 more sources
Geodesy and Geodynamics, 2021 The major earthquakes often trigger unrest of surrounding volcanic magma chambers. In recent years, three major earthquakes occurred around the Changbaishan volcano, but it was unclear whether these earthquakes triggered the unrest of the magma chamber ...
Dongzhen Wang +4 more
doaj +1 more source
Magma chamber decompression during explosive caldera-forming eruption of Aira caldera
Communications Earth & Environment, 2021 Decompression of a magma chamber is a fundamental condition of caldera collapse. Although theoretical models have predicted the decompression of magma chambers before caldera collapse, few previous studies have demonstrated the amount of magma chamber ...
N. Geshi +3 more
semanticscholar +1 more source
Magma chamber stratification of the 1815 Tambora caldera-forming eruption
Bulletin of Volcanology, 2021 The eruption of the Tambora volcano in 1815 was initiated by two precursory Plinian falls and formed two generations of pyroclastic density current (PDC) deposits. In this study, we found slight changes in phenocrysts (modal mineralogy, content, and size)
I. Suhendro +4 more
semanticscholar +1 more source