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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Bibliographic Details
Main Authors: Liu, Jiabo, Nowaczyk, Norbert R, Arz, Helge Wolfgang
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 2020
Subjects:
Black Sea
Laschamps
Mono Lake
Norwegian-Greenland Sea
Paleosecular variation
Baltic Sea Research Institute, Warnemünde IOW
GeoForschungszentrum Potsdam GFZ
Greenland
Greenland Sea
Online Access:https://dx.doi.org/10.1594/pangaea.919446
https://doi.pangaea.de/10.1594/PANGAEA.919446
Description
Summary: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 ...

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