Results 11 to 20 of about 579,075 (212)
Ardnamurchan 3D cone-sheet architecture explained by a single elongate magma chamber. [PDF]
Sci Rep, 2013 The Palaeogene Ardnamurchan central igneous complex, NW Scotland, was a defining place for the development of the classic concepts of cone-sheet and ring-dyke emplacement and has thus fundamentally influenced our thinking on subvolcanic structures.
Burchardt S +4 more
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Seismic Imaging of a Magma Chamber and Melt Recharge of the Dormant Datong Volcanoes [PDF]
Earth and Space Science, 2021 The Datong volcanoes erupted episodically from ca. 0.74 to ca 0.10 Ma with the last eruption at ca. 100 ka, and ever since has remained dormant. It remains elusive whether the Datong volcanoes are being recharged and would become active again in the near
Lipeng He +4 more
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On the Mechanical Effects of Poroelastic Crystal Mush in Classical Magma Chamber Models [PDF]
Journal of Geophysical Research: Solid Earth, 2018 Improved constraints on the mechanical behavior of magma chambers is essential for understanding volcanic processes; however, the role of crystal mush on the mechanical evolution of magma chambers has not yet been systematically studied.
Yang Liao, S. A. Soule, Max P. Jones
openalex +2 more sources
Magnetotelluric evidence for the deep causes of different eruptive styles of Changbaishan Tianchi and Longgang volcanoes [PDF]
Scientific ReportsLonggang Volcano (LGV) and Changbaishan Tianchi Volcano (CTV) share a common magmatic source at mantle depths. However, the two volcanoes have produced completely different types of eruptions.
Lingqiang Zhao +8 more
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Magma chamber failure and dyke injection threshold for magma-driven unrest at Campi Flegrei caldera [PDF]
Nature CommunicationsIn this work, we reconstruct the geometry and magma properties of the dyke that fed the Nisida eruption (~3.9 ka), located across the rim of the Campi Flegrei caldera (Italy). Results indicate that the magmatic overpressure was ~35 MPa, the dyke depth of
Jacopo Natale, Stefano Vitale
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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
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The shallow magma chamber of Stromboli Volcano (Italy)
Geophysical Research Letters, 2017 In this work, we integrate artificial and natural seismic sources data to obtain high‐resolution images of the shallow inner structure of Stromboli Volcano. Overall, we used a total of 21,953 P readings from an active seismic experiment and an additional
D. Patanè +8 more
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VolcanicaThis study utilizes 3D numerical models to simulate seismic resonances in a volcanic edifice, arising from the interaction between an externally excited wavefield and a magma chamber-conduit system.
Fabian Limberger, Georg Rümpker
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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
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