title: Palaeomagnetism of the Sarmatian-Maeotian of the Eastern Paratethys: Remagnetization or Not?
abstract: Abstract—We present the rock-magnetic and palaeomagnetic results of the Sarmatian-Maeotian (Upper Miocene) sediments of the key sections of Cape Popov Kamen and Cape Panagia from Taman Peninsula (Eastern Paratethys) and forming the flanks of a single synclinal fold. A three-component composition of magnetization has been detected. The first is the viscous component A, the second is the component B, which is intermediate between the components A and the third component C, which tends to zero in t
journal: Izvestiya Physics of the Solid Earth