IODP Expedition 378 Magnetic remanence (spinner)

Magnetic remanence was measured on discrete samples by an Agico JR-6A spinner magnetometer, first as natural remanent magnetization (NRM) and then after demagnetization or remagnetization steps were performed on the samples (e.g., alternating field [AF] demagnetization, thermal demagnetization [TD],...

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Bibliographic Details
Main Authors: Röhl, Ursula, Thomas, Deborah J., Childress, Laurel B., Anagnostou, Eleni, Ausín, Blanca, Boscolo Galazzo, Flavia, Dias, Bruna Borba, Brzelinski, Swaantje, Dunlea, Ann G., George, Simon C., Haynes, Laura L., Hendy, Ingrid L., Jones, Heather L., Khanolkar, Sonal S., Kitch, Gabriella D., Lee, Hojun, Raffi, Isabella, Reis, Alex J., Sheward, Rosie M., Sibert, Elizabeth, Tanaka, Erika, Wilkens, Roy H., Yasukawa, Kazutaka, Yuan, Wei, Zhang, Qiang, Zhang, Yang, Drury, Anna J., Hollis, Christopher J.
Other Authors: International Ocean Discovery Program
Format: Other/Unknown Material
Language:unknown
Published: International Ocean Discovery Program 2022
Subjects:
International Ocean Discovery Program
IODP
JOIDES Resolution
Expedition 378
Site U1553
South Pacific Paleogene Climate
climate and ocean change
Campbell Plateau
high southern latitude
carbon system dynamics
Cenozoic climate history
high CO2 world
chronostratigraphy
ocean circulation
intermediate water formation
hydrologic cycling
biological productivity
ice sheet dynamics
Pacific
Ice Sheet
Online Access:https://doi.org/10.5281/zenodo.10810024
Description
Summary:Magnetic remanence was measured on discrete samples by an Agico JR-6A spinner magnetometer, first as natural remanent magnetization (NRM) and then after demagnetization or remagnetization steps were performed on the samples (e.g., alternating field [AF] demagnetization, thermal demagnetization [TD], or isothermal remanent magnetization [IRM]).

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