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

Large‐scale faults in the continental crust are significant features that control the evolution of
sedimentary basins and intraplate mountain chains. Deciphering their evolution is a …

La Cordillera Ibérica es una cadena intraplaca formada durante el Paleógeno-Mioceno
inferior a partir de la inversión de la Cuenca Ibérica extensional mesozoica a partir de …

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

Abstract The Heart Mountain Slide in Wyoming is one of the largest known terrestrial gravity
slides (3,500 km2) formed∼ 49 Ma ago by the nearly horizontal detachment of Paleozoic …

This work aims to characterize the Gavarnie thrust, one of the large-scale thrusts that define
the Alpine structure of the west-central sector of the Pyrenees. A detailed comparison of …

AMS and structural analysis are here applied to study the deformed zone associated with a
large-scale, active normal fault in the central Betic Cordillera (Spain), namely the Baza fault …

The occurrence of a generalized remagnetization at 100 Ma makes the Cameros Basin, an 8
km thick Cretaceous extensional trough inverted during the Cenozoic, a perfect natural …

Heterogeneities in the magnetic signature along intraplate shear zones complicate their
correlation with the physical processes that are involved in the geodynamic evolution of …

Of the several factors involved in the development of magnetic fabrics in fault zones at
shallow crustal levels, lithology and deformation intensity have probably the most important …