10.1594/PANGAEA.925709Nowaczyk, Norbert RNorbert RNowaczykPANGAEA2020depositional remanent magnetizationMagnetic fieldDetrital remanent magnetization intensityDetrital remanent magnetizationComponents, magneticActionDataset10.1093/gji/ggaa455430 data pointstext/tab-separated-valuesCreative Commons Attribution 4.0 InternationalThis data publication provides data on redeposition experiments with mud collected during paleomagnetic sampling of various cores from the Arkhangelsky Ridge, SE Black Sea, recovered during marine expedition M72/5 of German research vessel RV METEOR in 2007 and expedition MSM33 of German research vessel RV Maria S. Merian in 2013. The collected silici-clastic mud mostly originates from glacial sediments deposited during marine isotope stages (MIS) 2 to 4, and 6. The material (bulk/mixed sample) originates from 208m to 847m water depth, 41° 28.66'N to 42° 13.57'N in latitude, and 36° 29.53'E to 37° 11.68'E in longitude. Experiments were performed in order to check the (non-) linearity of the detrital remanent magnetization (DRM) of Black Sea sediments acquired in different magnetic fields.Component(s) of the ambient magnetic field set by the coils system.
H - horizontal component
V – vertical component

vibr. - vibrating platform
still – still platform