(Table T1) Magnetic properties of ODP Hole 175-1081C

DOI

Magnetic properties are reported for samples from sediment cores recovered at Site 1081 on the Walvis Ridge (~20°S) during Leg 175 of the Ocean Drilling Program. Rock magnetic data indicate that the remanence is carried by low-coercivity minerals. Paramagnetic and diamagnetic minerals dominate the susceptibility. Comparison of measurements made aboard ship with those made on shore after the cruise indicate a marked loss of magnetization, probably due to dissolution of some magnetic minerals after core recovery similar to that which has occurred at other Leg 175 sites.

Supplement to: Frost, Gina Marie; Yamazaki, Toshitsugu (2001): Data report: Magnetic properties of core sediments from Site 1081 (Walvis Ridge), Leg 175. In: Wefer, G; Berger, WH; Richter, C (eds.) Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 175, 1-17

Identifier
DOI https://doi.org/10.1594/PANGAEA.787570
Related Identifier https://doi.org/10.2973/odp.proc.sr.175.206.2001
Metadata Access https://ws.pangaea.de/oai/provider?verb=GetRecord&metadataPrefix=datacite4&identifier=oai:pangaea.de:doi:10.1594/PANGAEA.787570
Provenance
Creator Frost, Gina Marie; Yamazaki, Toshitsugu
Publisher PANGAEA
Publication Year 2001
Rights Creative Commons Attribution 3.0 Unported; https://creativecommons.org/licenses/by/3.0/
OpenAccess true
Representation
Language English
Resource Type Supplementary Dataset; Dataset
Format text/tab-separated-values
Size 636 data points
Discipline Earth System Research
Spatial Coverage (11.319 LON, -19.620 LAT); Benguela Current, South Atlantic Ocean