Paleomagnetic results of sixteen Black Sea cores beween 68.9 and 14.5 ka ...
Paleomagnetic results derived from sixteen Black Sea sediment cores. The natural remanent magnetization (NRM) and the anhysteretic remanent magnetization (ARM) were measured with a 2G Enterprises 755 SRM (cryogenic) long-core magnetometer equipped with a sample holder for eight discrete samples at a...
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ftdatacite:10.1594/pangaea.919446 2024-09-15T18:09:51+00:00 Paleomagnetic results of sixteen Black Sea cores beween 68.9 and 14.5 ka ... Liu, Jiabo Nowaczyk, Norbert R Arz, Helge Wolfgang 2020 application/zip https://dx.doi.org/10.1594/pangaea.919446 https://doi.pangaea.de/10.1594/PANGAEA.919446 en eng PANGAEA https://dx.doi.org/10.1016/j.epsl.2018.04.014 https://dx.doi.org/10.1016/j.epsl.2018.12.029 https://dx.doi.org/10.1029/2019jb019225 https://dx.doi.org/10.1016/j.epsl.2012.06.050 https://dx.doi.org/10.1016/j.epsl.2013.09.028 https://dx.doi.org/10.1016/j.epsl.2017.12.009 https://dx.doi.org/10.1111/j.1365-246x.1980.tb02601.x Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 Black Sea Laschamps Mono Lake Norwegian-Greenland Sea Paleosecular variation Baltic Sea Research Institute, Warnemünde IOW GeoForschungszentrum Potsdam GFZ article Bundled Publication of Datasets Collection 2020 ftdatacite https://doi.org/10.1594/pangaea.91944610.1016/j.epsl.2018.04.01410.1016/j.epsl.2018.12.02910.1029/2019jb01922510.1016/j.epsl.2012.06.05010.1016/j.epsl.2013.09.02810.1016/j.epsl.2017.12.00910.1111/j.1365-246x.1980.tb02601.x 2024-07-03T13:15:54Z Paleomagnetic results derived from sixteen Black Sea sediment cores. The natural remanent magnetization (NRM) and the anhysteretic remanent magnetization (ARM) were measured with a 2G Enterprises 755 SRM (cryogenic) long-core magnetometer equipped with a sample holder for eight discrete samples at a separation of 20 cm. The magnetometer's in-line tri-axial alternating field (AF) demagnetizer was used to demagnetize the NRM and ARM of the samples. The NRM was measured after application of AF peak amplitudes of 0, 5, 10, 15, 20, 30, 40, 50, 65, 80, and 100 mT. Directions of the characteristic remanent magnetization (ChRM) were determined by principle component analysis (PCA) according to Kirschvink (1980). The error range of the ChRM is given as the maximum angular deviation (MAD). The ARM was imparted along the samples' z-axis with a static field of 0.05 mT and an AF field of 100 mT. Demagnetization then was performed in steps of 0, 10, 20, 30, 40, 50, 65, and 80 mT. The median destructive field of the ARM ... Article in Journal/Newspaper Greenland Greenland Sea DataCite |
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English |
topic |
Black Sea Laschamps Mono Lake Norwegian-Greenland Sea Paleosecular variation Baltic Sea Research Institute, Warnemünde IOW GeoForschungszentrum Potsdam GFZ |
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Black Sea Laschamps Mono Lake Norwegian-Greenland Sea Paleosecular variation Baltic Sea Research Institute, Warnemünde IOW GeoForschungszentrum Potsdam GFZ Liu, Jiabo Nowaczyk, Norbert R Arz, Helge Wolfgang Paleomagnetic results of sixteen Black Sea cores beween 68.9 and 14.5 ka ... |
topic_facet |
Black Sea Laschamps Mono Lake Norwegian-Greenland Sea Paleosecular variation Baltic Sea Research Institute, Warnemünde IOW GeoForschungszentrum Potsdam GFZ |
description |
Paleomagnetic results derived from sixteen Black Sea sediment cores. The natural remanent magnetization (NRM) and the anhysteretic remanent magnetization (ARM) were measured with a 2G Enterprises 755 SRM (cryogenic) long-core magnetometer equipped with a sample holder for eight discrete samples at a separation of 20 cm. The magnetometer's in-line tri-axial alternating field (AF) demagnetizer was used to demagnetize the NRM and ARM of the samples. The NRM was measured after application of AF peak amplitudes of 0, 5, 10, 15, 20, 30, 40, 50, 65, 80, and 100 mT. Directions of the characteristic remanent magnetization (ChRM) were determined by principle component analysis (PCA) according to Kirschvink (1980). The error range of the ChRM is given as the maximum angular deviation (MAD). The ARM was imparted along the samples' z-axis with a static field of 0.05 mT and an AF field of 100 mT. Demagnetization then was performed in steps of 0, 10, 20, 30, 40, 50, 65, and 80 mT. The median destructive field of the ARM ... |
format |
Article in Journal/Newspaper |
author |
Liu, Jiabo Nowaczyk, Norbert R Arz, Helge Wolfgang |
author_facet |
Liu, Jiabo Nowaczyk, Norbert R Arz, Helge Wolfgang |
author_sort |
Liu, Jiabo |
title |
Paleomagnetic results of sixteen Black Sea cores beween 68.9 and 14.5 ka ... |
title_short |
Paleomagnetic results of sixteen Black Sea cores beween 68.9 and 14.5 ka ... |
title_full |
Paleomagnetic results of sixteen Black Sea cores beween 68.9 and 14.5 ka ... |
title_fullStr |
Paleomagnetic results of sixteen Black Sea cores beween 68.9 and 14.5 ka ... |
title_full_unstemmed |
Paleomagnetic results of sixteen Black Sea cores beween 68.9 and 14.5 ka ... |
title_sort |
paleomagnetic results of sixteen black sea cores beween 68.9 and 14.5 ka ... |
publisher |
PANGAEA |
publishDate |
2020 |
url |
https://dx.doi.org/10.1594/pangaea.919446 https://doi.pangaea.de/10.1594/PANGAEA.919446 |
genre |
Greenland Greenland Sea |
genre_facet |
Greenland Greenland Sea |
op_relation |
https://dx.doi.org/10.1016/j.epsl.2018.04.014 https://dx.doi.org/10.1016/j.epsl.2018.12.029 https://dx.doi.org/10.1029/2019jb019225 https://dx.doi.org/10.1016/j.epsl.2012.06.050 https://dx.doi.org/10.1016/j.epsl.2013.09.028 https://dx.doi.org/10.1016/j.epsl.2017.12.009 https://dx.doi.org/10.1111/j.1365-246x.1980.tb02601.x |
op_rights |
Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 |
op_doi |
https://doi.org/10.1594/pangaea.91944610.1016/j.epsl.2018.04.01410.1016/j.epsl.2018.12.02910.1029/2019jb01922510.1016/j.epsl.2012.06.05010.1016/j.epsl.2013.09.02810.1016/j.epsl.2017.12.00910.1111/j.1365-246x.1980.tb02601.x |
_version_ |
1810447445891481600 |