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 …

Integration of structural, stratigraphic, and paleomagnetic data from the N–S trending
structures of the Ainsa Oblique Zone reveals the kinematics of the major thrust salient in the …

Remagnetization of a palaeomagnetic signal is difficult to recognize independently of
directional information. The situation becomes more complex when remagnetized rocks …

Authigenic formation of fine-grained magnetite is responsible for widespread chemical
remagnetization of many carbonate rocks. Authigenic magnetite grains, dominantly in the …

Abstract The Tibetan Himalaya represents the northernmost continental unit of the Indian
plate that collided with Asia in the Cenozoic. Paleomagnetic studies on the Tibetan …

Here we present a detailed study of the magnetic fabrics and subfabrics of remagnetized
Upper Cretaceous limolites that crop out in the Internal Sierras (west central Pyrenees) …

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 …

This chapter presents the results of numerous rock experiments carried out on Jurassic
marine carbonates and red beds from the Central High Atlas, which have been affected by a …

In this paper, we present the first palaeomagnetic data (51 sites) for Mesozoic (Lower–
Middle Jurassic) sediments of the Moroccan Central High Atlas and address the study of a …

Paleomagnetism is a technique very useful in structural geology providing that the rocks
keep a stable record of the paleoearth magnetic field information. Paleomagnetism has …