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author Bukar, Shettima
von Dobeneck, Tilo
author_facet Bukar, Shettima
von Dobeneck, Tilo
collection Datos científicos de ciencias marinas y ambientales
contents In order to determine the bulk magnetic impact of all 22 classified IRD lithologies, the specific petromagnetic properties of each were investigated in detail. In order to represent host rock composition as good as possible and to meet the magnetometric sensitivity requirements, the largest available IRD particles (dropstones) of each IRD species were selected, that were typically of granule or pebble size. Where such large particles were not available, several petrologically similar coarse sand-sized particles were combined in one sample. Great care was taken in sample preparation and sample holder correction to reach reliable values even for small and low-magnetic samples. In addition to magnetic properties, we also provide averaged IRD counts of HLs and in ILs for each IRD lithology.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_971696
institution PANGAEA
language en
publishDate 2025
publisher PANGAEA
record_format pangaea
spellingShingle Rock magnetic properties of petrologically representative IRD particles in sediment core GeoB18530-1
Bukar, Shettima
von Dobeneck, Tilo
509-1; ArcTrain; Counting >1000 µm fraction; GC; GeoB18530-1; Geochemistry; grain size distribution; Grand Banks Margin; Gravity corer; Hard isothermal remanent magnetization; Heinrich events; Ice rafted detritus; Ice-Rafted Detritus; Isothermal remanent magnetization, mass-normalized; Kappabridge, AGICO KLY-2; Lithology/composition/facies; Magnetic susceptibility; Magnetometer, cryogenic, pass-through, 2G Enterprises 755 R; Maria S. Merian; MSM39; Processes and impacts of climate change in the North Atlantic Ocean and the Canadian Arctic; rock magnetism; Saturation isothermal remanent magnetization/kappa ratio; SE Grand Banks Slope; S-ratio; Stereo microscope, Zeiss, Stemi
In order to determine the bulk magnetic impact of all 22 classified IRD lithologies, the specific petromagnetic properties of each were investigated in detail. In order to represent host rock composition as good as possible and to meet the magnetometric sensitivity requirements, the largest available IRD particles (dropstones) of each IRD species were selected, that were typically of granule or pebble size. Where such large particles were not available, several petrologically similar coarse sand-sized particles were combined in one sample. Great care was taken in sample preparation and sample holder correction to reach reliable values even for small and low-magnetic samples. In addition to magnetic properties, we also provide averaged IRD counts of HLs and in ILs for each IRD lithology.
title Rock magnetic properties of petrologically representative IRD particles in sediment core GeoB18530-1
topic 509-1; ArcTrain; Counting >1000 µm fraction; GC; GeoB18530-1; Geochemistry; grain size distribution; Grand Banks Margin; Gravity corer; Hard isothermal remanent magnetization; Heinrich events; Ice rafted detritus; Ice-Rafted Detritus; Isothermal remanent magnetization, mass-normalized; Kappabridge, AGICO KLY-2; Lithology/composition/facies; Magnetic susceptibility; Magnetometer, cryogenic, pass-through, 2G Enterprises 755 R; Maria S. Merian; MSM39; Processes and impacts of climate change in the North Atlantic Ocean and the Canadian Arctic; rock magnetism; Saturation isothermal remanent magnetization/kappa ratio; SE Grand Banks Slope; S-ratio; Stereo microscope, Zeiss, Stemi
url https://doi.org/10.1594/PANGAEA.971696