The use of the Anisotropy of Magnetic Susceptibility (AMS) has become a rather common
practice in Earth Sciences since the pioneer note by Graham. The versatility of the …

The kinematic evolution of the Pyrenees was largely controlled by structural and thermal
heterogeneities inherited from a precursor rift system, resulting in complex along-strike …

Magnetic fabric analysis is a common technique to assess the strain regime during mountain
building processes. Here, we use this approach to evaluate the tectonic evolution of the …

In orogenic systems, thrust faults play a major role in stacking different tectonic units and
may act as conduits for the expulsion of large amounts of fluid of different origins …

During compressive events, deformation in sedimentary basins is mainly accommodated by
thrust faulting and related fold growth. Thrust faults are generally rooted in the basement and …

Positive tectonic inversion of sedimentary basins has been recognized as one of the primary
mechanisms of mountain building and intraplate deformation. Reconstructing the tectonic …

Abstract The Sanmenxia Basin, located on the southeastern margin of the Shanxi rift and
filled with Cretaceous-Paleogene fluvial and lacustrine sediments, is a faulted basin …

Sedimentological, geochemical and magnetic data in a~ 7-m sequence from Marboré Lake
(2612 m asl, central Pyrenees) provide information about environmental variability since the …

The transition between extensional and compressional-driven magnetic fabrics in
sedimentary rocks is explored in this paper through the study of an example of the Basque …

Anisotropy of magnetic susceptibility (AMS) has been applied to the study of shallow fault
zones, although interpretation of the results requires establishing clear relationships …