Magnetic fabrics in the turbidite deposits of the Central Carpathian Paleogene Basin in relation to sedimentary and tectonic fabric elements

Late and post-collisional tectonic evolution of the Adria-Europe suture in the Vardar Zone

“…It is interesting to note that the magnetite which is the carrier of the ChRM in the flysch and probably produced from pyrite (e.g. Brothers et al, 1996, Madzin et al, 2021 must have existed during Late Cretaceous-Eocene compression. The evidence for this is that the AARM (anisotropy of the remanence) foliation planes and lineation directions (Fig.…”