This study was supported by grants from the Israeli Government under Geological Survey of Israel DS project 40706, and the Israel Science Foundation (ISF grants 868/17). We are indebted to Vladimir Lyakhovsky for helpful discussions during the course of this study, and to Mike Jackson, Bjarne Almqvist, and Jason Patton for providing constructive and very helpful reviewsPeer reviewedPostprin
Of the several factors involved in the development of magnetic fabrics in fault zones at shallow cru...
The anisotropy of magnetic susceptibility (AMS) study was performed on soft sediment samples from a ...
The analysis of the Anisotropy of Magnetic Susceptibility (AMS) constitutes a fast and non-destructi...
The anisotropy of magnetic susceptibility (AMS) of soft rocks was measured in order to dis-tinguish ...
International audienceOff-fault seismogenic deformation in sediments (seismites) has proved useful f...
International audienceClastic dikes may form by simultaneous fracture propagation in rocks and injec...
International audienceClastic dikes form either by passive deposition of clastic material into preex...
As a petrofabric indicator, anisotropy of magnetic susceptibility (AMS) can potentially be used to i...
Acknowledgements This study was supported by the Israel Science Foundation (ISF grants 868/17) and a...
AbstractSoft-sediment deformation structures induced by seismic liquefaction and/or fluidization rec...
Soft-sediment deformation structures induced by seismic liquefaction and/or fluidization receive muc...
Major discontinuities in the Earth’s crust are expressed by faults that often cut across its whole t...
This study was supported by the Israel Science Foundation (ISF grants No. 1245/11 and 1436/14). We t...
The Pelham gneiss dome in northern Massachusetts ultimately developed during the Appalachian Mountai...
Author Posting. © American Geophysical Union, 2007. This article is posted here by permission of Am...
Of the several factors involved in the development of magnetic fabrics in fault zones at shallow cru...
The anisotropy of magnetic susceptibility (AMS) study was performed on soft sediment samples from a ...
The analysis of the Anisotropy of Magnetic Susceptibility (AMS) constitutes a fast and non-destructi...
The anisotropy of magnetic susceptibility (AMS) of soft rocks was measured in order to dis-tinguish ...
International audienceOff-fault seismogenic deformation in sediments (seismites) has proved useful f...
International audienceClastic dikes may form by simultaneous fracture propagation in rocks and injec...
International audienceClastic dikes form either by passive deposition of clastic material into preex...
As a petrofabric indicator, anisotropy of magnetic susceptibility (AMS) can potentially be used to i...
Acknowledgements This study was supported by the Israel Science Foundation (ISF grants 868/17) and a...
AbstractSoft-sediment deformation structures induced by seismic liquefaction and/or fluidization rec...
Soft-sediment deformation structures induced by seismic liquefaction and/or fluidization receive muc...
Major discontinuities in the Earth’s crust are expressed by faults that often cut across its whole t...
This study was supported by the Israel Science Foundation (ISF grants No. 1245/11 and 1436/14). We t...
The Pelham gneiss dome in northern Massachusetts ultimately developed during the Appalachian Mountai...
Author Posting. © American Geophysical Union, 2007. This article is posted here by permission of Am...
Of the several factors involved in the development of magnetic fabrics in fault zones at shallow cru...
The anisotropy of magnetic susceptibility (AMS) study was performed on soft sediment samples from a ...
The analysis of the Anisotropy of Magnetic Susceptibility (AMS) constitutes a fast and non-destructi...