Investigating the possible effects of salt in the fault zones on rates of seismicity - insights from analogue and numerical modeling

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Location: Deutsche Nationalbibliothek Frankfurt am Main

Extent: Online-Ressource

Language: Englisch

Notes: In: Katlenburg-Lindau : European Geophysical Society, 2017 (Geophysical Research Abstracts; 19), Seiten/Artikel-Nr:EGU2017-13631, 1 Seite

Classification: Geowissenschaften

Event: Veröffentlichung

(where): Aachen

(who): Universitätsbibliothek der RWTH Aachen

(when): 2017

Creator: Urai, Janos
Kettermann, Michael
Abe, Steffen

DOI: 10.18154/RWTH-2018-230909

URN: urn:nbn:de:101:1-2019032106152261381253

Rights: Der Zugriff auf das Objekt ist unbeschränkt möglich.

Last update: 25.03.2025, 1:48 PM CET

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Associated

Urai, Janos
Kettermann, Michael
Abe, Steffen
Universitätsbibliothek der RWTH Aachen

Time of origin

2017

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Deformation in layered Zechstein-III K-Mg salts with high mechanical contrasts. Core analysis revealing strain concentrations and the development of fracturing and folding into a tectonic mélange

The microvein dilemma

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Investigating the possible effects of salt in the fault zones on rates of seismicity - insights from analogue and numerical modeling

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Other Objects (12)

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Rheological stratification in Zechstein rock salt caused by thermodynamically controlled reorganization of grain boundary fluids? : A test using gravitationally induced sinking of anhydrite-dolomite stringers

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Crack - seal veins - what we learnt since the seminal work of John Ramsay

Internal deformation in layered Zechstein-III K-Mg salts : Structures formed by complex deformation and high contrasts in viscosity observed in drill cores

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How rheological heterogeneities control the internal deformation of salt giants

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Crack - seal veins - what we learnt since the seminal work of John Ramsay

Internal deformation in layered Zechstein-III K-Mg salts : Structures formed by complex deformation and high contrasts in viscosity observed in drill cores

Deformation in layered Zechstein-III K-Mg salts with high mechanical contrasts. Core analysis revealing strain concentrations and the development of fracturing and folding into a tectonic mélange

The microvein dilemma

Influence of obliquity on the geometry of massively dilatant faults - insights from scaled analogue models

Microstructures and deformation mechanisms in Opalinus Clay: insights from scaly clay from the Main Fault in the Mont Terri Rock Laboratory (CH)

Fault gouge in sand-clay sequences - a first look in 3D

Normal faulting in basalts with vertical cooling joints: lessons learned from analogue models and outcrop studies in Iceland

Rheological stratification in Zechstein rock salt caused by thermodynamically controlled reorganization of grain boundary fluids? : A test using gravitationally induced sinking of anhydrite-dolomite stringers

Syn-depositional deformation of the late Zechstein evaporites on the Friesland Platform capturing the early life of a salt giant

How rheological heterogeneities control the internal deformation of salt giants

Rheology of rock salt for salt tectonics modeling

Crack - seal veins - what we learnt since the seminal work of John Ramsay

Internal deformation in layered Zechstein-III K-Mg salts : Structures formed by complex deformation and high contrasts in viscosity observed in drill cores

Deformation in layered Zechstein-III K-Mg salts with high mechanical contrasts. Core analysis revealing strain concentrations and the development of fracturing and folding into a tectonic mélange

The microvein dilemma

Influence of obliquity on the geometry of massively dilatant faults - insights from scaled analogue models

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