Dynamic pressure variations in the lower crust caused by localized fluid-induced weakening

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Location: Deutsche Nationalbibliothek Frankfurt am Main

ISSN: 2662-4435

Extent: Online-Ressource

Language: Englisch

Notes: online resource.

Bibliographic citation: Dynamic pressure variations in the lower crust caused by localized fluid-induced weakening ; volume:3 ; number:1 ; day:8 ; month:7 ; year:2022 ; pages:1-7 ; date:12.2022
Communications earth & environment ; 3, Heft 1 (8.7.2022), 1-7, 12.2022

Creator: Moulas, Evangelos
Kaus, Boris Jozef Paul
Jamtveit, Bjørn

Contributor: SpringerLink (Online service)

DOI: 10.1038/s43247-022-00478-7

URN: urn:nbn:de:101:1-2022083019251352915471

Rights: Open Access; Der Zugriff auf das Objekt ist unbeschränkt möglich.

Last update: 15.08.2025, 7:29 AM CEST

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Moulas, Evangelos
Kaus, Boris Jozef Paul
Jamtveit, Bjørn
SpringerLink (Online service)

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Estimating weakening on hillslopes caused by strong earthquakes

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High Pressure Metamorphism Caused by Fluid Induced Weakening of Deep Continental Crust

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Estimating weakening on hillslopes caused by strong earthquakes

Fluid reservoirs in the crust and mechanical coupling between the upper and lower crust

Rapid hydration and weakening of anhydrite under stress: implications for natural hydration in the Earth's crust and mantle

Imposed strain localization in the lower crust on seismic timescales

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Dynamic pressure variations in the lower crust caused by localized fluid-induced weakening

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Other Objects (12)

High Pressure Metamorphism Caused by Fluid Induced Weakening of Deep Continental Crust

Fault weakening caused by smectite swelling

Estimating weakening on hillslopes caused by strong earthquakes

Fluid reservoirs in the crust and mechanical coupling between the upper and lower crust

Rapid hydration and weakening of anhydrite under stress: implications for natural hydration in the Earth's crust and mantle

Imposed strain localization in the lower crust on seismic timescales

CRUSt

"CRUSt"

CRUSt

CRUST

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High Pressure Metamorphism Caused by Fluid Induced Weakening of Deep Continental Crust

Fault weakening caused by smectite swelling

Estimating weakening on hillslopes caused by strong earthquakes

Fluid reservoirs in the crust and mechanical coupling between the upper and lower crust

Rapid hydration and weakening of anhydrite under stress: implications for natural hydration in the Earth's crust and mantle

Imposed strain localization in the lower crust on seismic timescales

CRUSt

"CRUSt"

CRUSt

CRUST

CRUSt

CRUSt

High Pressure Metamorphism Caused by Fluid Induced Weakening of Deep Continental Crust

Fault weakening caused by smectite swelling

Estimating weakening on hillslopes caused by strong earthquakes

Fluid reservoirs in the crust and mechanical coupling between the upper and lower crust

Rapid hydration and weakening of anhydrite under stress: implications for natural hydration in the Earth's crust and mantle

Imposed strain localization in the lower crust on seismic timescales

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"CRUSt"

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