Inversion tectonics and magnetic fabrics in Mesozoic basins of the Western Tethys: A review
Positive tectonic inversion of sedimentary basins has been recognized as one of the primary
mechanisms of mountain building and intraplate deformation. Reconstructing the tectonic …
mechanisms of mountain building and intraplate deformation. Reconstructing the tectonic …
Inverse magnetic fabric in carbonate-bearing rocks
P Rochette - Earth and Planetary Science Letters, 1988 - Elsevier
The observation of a magnetic susceptibility ellipsoid whose maximum axis corresponds to
the minimum axis of petrofabric (pole of bedding or schistosity) is referred to as an inverse …
the minimum axis of petrofabric (pole of bedding or schistosity) is referred to as an inverse …
Magnetic fabric of weakly deformed clay-rich sediments in the Italian peninsula: relationship with compressional and extensional tectonics
We present the results of anisotropy of magnetic susceptibility (AMS) analyses carried out in
weakly deformed Neogene and Quaternary clay-rich sediments from different compressional …
weakly deformed Neogene and Quaternary clay-rich sediments from different compressional …
Magnetic fabric as a structural indicator of the deformation path within a fold-thrust structure: a test case from the Corbières (NE Pyrenees, France)
O Averbuch, DF de Lamotte, C Kissel - Journal of Structural Geology, 1992 - Elsevier
In order to define the deformation path and the distribution of internal deformation in a
foreland foldthrust structure, the anisotropy of magnetic susceptibility was measured in 150 …
foreland foldthrust structure, the anisotropy of magnetic susceptibility was measured in 150 …
The origin of tectonic lineation in extensional basins: combined neutron texture and magnetic analyses on “undeformed” clays
In extensional sedimentary basins fine-grained sediments that appear undeformed at the
outcrop scale can carry a magnetic fabric consistent with the regional deformation pattern …
outcrop scale can carry a magnetic fabric consistent with the regional deformation pattern …
Magnetic fabric of clay sediments from the external northern Apennines (Italy)
We report on the anisotropy of magnetic susceptibility (AMS) analyses of fine-grained
sediments deposited during the Messinian in foredeep basins at the front of the northern …
sediments deposited during the Messinian in foredeep basins at the front of the northern …
Anisotropy of magnetic susceptibility in weakly deformed red beds from the Wyoming salient, Sevier thrust belt: Relations to layer-parallel shortening and orogenic …
Anisotropy of magnetic susceptibility (AMS) and structural studies of red beds in the
Wyoming salient were completed to evaluate relations of magnetic fabrics to layer-parallel …
Wyoming salient were completed to evaluate relations of magnetic fabrics to layer-parallel …
A Late Cretaceous true polar wander oscillation
True polar wander (TPW), or planetary reorientation, is well documented for other planets
and moons and for Earth at present day with satellites, but testing its prevalence in Earth's …
and moons and for Earth at present day with satellites, but testing its prevalence in Earth's …
Extensional tectonics on Sardinia (Italy): insights into the arc–back-arc transitional regime
Although the tectonic features and stress regime typical for accretionary complexes and
back-arc domains have been widely documented so far, few are known on the transitional …
back-arc domains have been widely documented so far, few are known on the transitional …
First paleomagnetic evidence for a post-Eocene clockwise rotation of the Western Taurides thrust belt east of the Isparta reentrant (Southwestern Turkey)
C Kissel, O Averbuch, DF de Lamotte, O Monod… - Earth and Planetary …, 1993 - Elsevier
A paleomagnetic study was carried out on 23 sites sampled in Paleocene, Eocene and
Lower Miocene sedimentary formations of the Western Taurides belt east of the Isparta …
Lower Miocene sedimentary formations of the Western Taurides belt east of the Isparta …