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COMSOL Inc multiphysics deformation model
Results of the COMSOL <t>Multiphysics</t> deformation model simulating the effects of the observed roof subsidence on the east side of the Rílutungnahamrar–Fálkahnaus conduit. ( a ) X–Z cross section. Subsidence is localized to a zone close to the dyke. Black lines indicate the tilt of previously horizontal lines (i.e. lava layers). ( b ) Subsidence of the pluton roof at the pluton roof interface. The black box marks the zone which was forced to subside. The dyke is located at the left edge of the black box. ( c ) Subsidence observed at the Earth’s surface (i.e. 1.75 km above the pluton roof). The black box indicates the pluton extents in the model.
Multiphysics Deformation Model, supplied by COMSOL Inc, used in various techniques. Bioz Stars score: 90/100, based on 1 PubMed citations. ZERO BIAS - scores, article reviews, protocol conditions and more
https://www.bioz.com/result/multiphysics deformation model/product/COMSOL Inc
Average 90 stars, based on 1 article reviews
multiphysics deformation model - by Bioz Stars, 2026-06
90/100 stars

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1) Product Images from "Volcanic unrest as seen from the magmatic source: Reyðarártindur pluton, Iceland"

Article Title: Volcanic unrest as seen from the magmatic source: Reyðarártindur pluton, Iceland

Journal: Scientific Reports

doi: 10.1038/s41598-023-50880-0

Results of the COMSOL Multiphysics deformation model simulating the effects of the observed roof subsidence on the east side of the Rílutungnahamrar–Fálkahnaus conduit. ( a ) X–Z cross section. Subsidence is localized to a zone close to the dyke. Black lines indicate the tilt of previously horizontal lines (i.e. lava layers). ( b ) Subsidence of the pluton roof at the pluton roof interface. The black box marks the zone which was forced to subside. The dyke is located at the left edge of the black box. ( c ) Subsidence observed at the Earth’s surface (i.e. 1.75 km above the pluton roof). The black box indicates the pluton extents in the model.
Figure Legend Snippet: Results of the COMSOL Multiphysics deformation model simulating the effects of the observed roof subsidence on the east side of the Rílutungnahamrar–Fálkahnaus conduit. ( a ) X–Z cross section. Subsidence is localized to a zone close to the dyke. Black lines indicate the tilt of previously horizontal lines (i.e. lava layers). ( b ) Subsidence of the pluton roof at the pluton roof interface. The black box marks the zone which was forced to subside. The dyke is located at the left edge of the black box. ( c ) Subsidence observed at the Earth’s surface (i.e. 1.75 km above the pluton roof). The black box indicates the pluton extents in the model.

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Results of the COMSOL <t>Multiphysics</t> deformation model simulating the effects of the observed roof subsidence on the east side of the Rílutungnahamrar–Fálkahnaus conduit. ( a ) X–Z cross section. Subsidence is localized to a zone close to the dyke. Black lines indicate the tilt of previously horizontal lines (i.e. lava layers). ( b ) Subsidence of the pluton roof at the pluton roof interface. The black box marks the zone which was forced to subside. The dyke is located at the left edge of the black box. ( c ) Subsidence observed at the Earth’s surface (i.e. 1.75 km above the pluton roof). The black box indicates the pluton extents in the model.
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Results of the COMSOL <t>Multiphysics</t> deformation model simulating the effects of the observed roof subsidence on the east side of the Rílutungnahamrar–Fálkahnaus conduit. ( a ) X–Z cross section. Subsidence is localized to a zone close to the dyke. Black lines indicate the tilt of previously horizontal lines (i.e. lava layers). ( b ) Subsidence of the pluton roof at the pluton roof interface. The black box marks the zone which was forced to subside. The dyke is located at the left edge of the black box. ( c ) Subsidence observed at the Earth’s surface (i.e. 1.75 km above the pluton roof). The black box indicates the pluton extents in the model.
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Results of the COMSOL Multiphysics deformation model simulating the effects of the observed roof subsidence on the east side of the Rílutungnahamrar–Fálkahnaus conduit. ( a ) X–Z cross section. Subsidence is localized to a zone close to the dyke. Black lines indicate the tilt of previously horizontal lines (i.e. lava layers). ( b ) Subsidence of the pluton roof at the pluton roof interface. The black box marks the zone which was forced to subside. The dyke is located at the left edge of the black box. ( c ) Subsidence observed at the Earth’s surface (i.e. 1.75 km above the pluton roof). The black box indicates the pluton extents in the model.

Journal: Scientific Reports

Article Title: Volcanic unrest as seen from the magmatic source: Reyðarártindur pluton, Iceland

doi: 10.1038/s41598-023-50880-0

Figure Lengend Snippet: Results of the COMSOL Multiphysics deformation model simulating the effects of the observed roof subsidence on the east side of the Rílutungnahamrar–Fálkahnaus conduit. ( a ) X–Z cross section. Subsidence is localized to a zone close to the dyke. Black lines indicate the tilt of previously horizontal lines (i.e. lava layers). ( b ) Subsidence of the pluton roof at the pluton roof interface. The black box marks the zone which was forced to subside. The dyke is located at the left edge of the black box. ( c ) Subsidence observed at the Earth’s surface (i.e. 1.75 km above the pluton roof). The black box indicates the pluton extents in the model.

Article Snippet: Figure 8 Results of the COMSOL Multiphysics deformation model simulating the effects of the observed roof subsidence on the east side of the Rílutungnahamrar–Fálkahnaus conduit. ( a ) X–Z cross section.

Techniques: