IODP Expedition 360 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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Bibliographische Detailangaben
Hauptverfasser:	Dick, Henry J.B., MacLeod, Christopher J., Blum, Peter, Abe, Natsue, Blackman, Donna K., Bowles, Julie A., Cheadle, Michael J., Cho, Kyungo, Ciazela, Jakub, Deans, Jeremy R., Edgcomb, Virginia P., Ferrando, Carlotta, France, Lyderic, Ghosh, Biswajit, Ildefonse, Benoit, Kendrick, Mark A., Koepke, Juergen H., Leong, James A.M., Liu, Chuanzhou, Ma, Qiang, Morishita, Tomoaki, Morris, Antony, Natland, James H., Nozaka, Toshio, Pluemper, Oliver, Sanfilippo, Alessio, Sylvan, Jason B., Tivey, Maurice A, Tribuzio, Riccardo, Viegas, Luis G.F.
Format:	Dataset
Sprache:	eng
Schlagworte:	Atlantis Bank Atlantis II Transform Earth connections Expedition 360 Hole 1105A International Ocean Discovery Program IODP JOIDES Resolution mid-ocean ridge Moho Mohorovicic discontinuity Site U1473 SloMo slow spreading ridge Southwest Indian Ridge upper mantle
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Beschreibung
Zusammenfassung:	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]).
DOI:	10.5281/zenodo.11984455