The Effect of Obliquity of Slip in Normal Faults on Distribution of Open Fractures
- Standort
-
Deutsche Nationalbibliothek Frankfurt am Main
- Umfang
-
Online-Ressource
- Sprache
-
Englisch
- Erschienen in
-
In: 10.3389/feart.2019.00018
- Klassifikation
-
Geowissenschaften
- Ereignis
-
Veröffentlichung
- (wo)
-
Aachen
- (wer)
-
Universitätsbibliothek der RWTH Aachen
- (wann)
-
2019
- Urheber
-
Hagke, Johann-Christoph von
Kettermann, Michael
Bitsch, Nicolai
Bücken, Daniel
Weismüller, Christopher
Urai, Janos
- DOI
-
10.18154/RWTH-2019-05094
- URN
-
urn:nbn:de:101:1-2019082906323484938361
- Rechteinformation
-
Der Zugriff auf das Objekt ist unbeschränkt möglich.
- Letzte Aktualisierung
-
15.08.2025, 07:38 MESZ
Datenpartner
Dieses Objekt wird bereitgestellt von:
Deutsche Nationalbibliothek. Bei Fragen zum Objekt wenden Sie sich bitte an den Datenpartner.
Deutsche Nationalbibliothek. Bei Fragen zum Objekt wenden Sie sich bitte an den Datenpartner.
Beteiligte
- Hagke, Johann-Christoph von
- Kettermann, Michael
- Bitsch, Nicolai
- Bücken, Daniel
- Weismüller, Christopher
- Urai, Janos
- Universitätsbibliothek der RWTH Aachen
Entstanden
- 2019
Ähnliche Objekte (12)
Abutting faults: a case study of the evolution of strain at Courthouse branch point, Moab Fault, Utah
Abutting faults: a case study of the evolution of strain at Courthouse branch point, Moab Fault, Utah
Fractures and faults in tight gas sandstones : a study using laboratory and field data
Rheology of rock salt for salt tectonics modeling
Syn-depositional deformation of the late Zechstein evaporites on the Friesland Platform capturing the early life of a salt giant
Influence of obliquity on the geometry of massively dilatant faults - insights from scaled analogue models
How rheological heterogeneities control the internal deformation of salt giants
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
Mapping of massively dilatant faults in Iceland using UAV-SfM and TLS
Crack - seal veins - what we learnt since the seminal work of John Ramsay
Multiphase boudinage: a case study of amphibolites in marble in the Naxos migmatite core
Structure of massively dilatant faults in Iceland: lessons learned from high resolution UAV data
Abutting faults: a case study of the evolution of strain at Courthouse branch point, Moab Fault, Utah
Abutting faults: a case study of the evolution of strain at Courthouse branch point, Moab Fault, Utah
Fractures and faults in tight gas sandstones : a study using laboratory and field data
Rheology of rock salt for salt tectonics modeling
Syn-depositional deformation of the late Zechstein evaporites on the Friesland Platform capturing the early life of a salt giant
Influence of obliquity on the geometry of massively dilatant faults - insights from scaled analogue models
How rheological heterogeneities control the internal deformation of salt giants
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
Mapping of massively dilatant faults in Iceland using UAV-SfM and TLS
Crack - seal veins - what we learnt since the seminal work of John Ramsay
Multiphase boudinage: a case study of amphibolites in marble in the Naxos migmatite core
Structure of massively dilatant faults in Iceland: lessons learned from high resolution UAV data
Abutting faults: a case study of the evolution of strain at Courthouse branch point, Moab Fault, Utah
Abutting faults: a case study of the evolution of strain at Courthouse branch point, Moab Fault, Utah
Fractures and faults in tight gas sandstones : a study using laboratory and field data
Rheology of rock salt for salt tectonics modeling
Syn-depositional deformation of the late Zechstein evaporites on the Friesland Platform capturing the early life of a salt giant
Influence of obliquity on the geometry of massively dilatant faults - insights from scaled analogue models
How rheological heterogeneities control the internal deformation of salt giants
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
Mapping of massively dilatant faults in Iceland using UAV-SfM and TLS
Crack - seal veins - what we learnt since the seminal work of John Ramsay
Multiphase boudinage: a case study of amphibolites in marble in the Naxos migmatite core