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.
1 Frost, G.M., and Yamazaki, T., 2001. Data report: Magnetic properties of core sediments from Site 1081 (Walvis Ridge), Leg 175. In Wefer, G., Berger, W.H., and Richter, C. (Eds.), Proc. ODP, Sci. Results, 175 [Online]. Available from World Wide Web: <http://www-odp.tamu.edu/publications/175_SR/chap_08/chap_08.htm>. [Cited YYYY-MM-DD]
2 Hawaii Institute of Geophysics and Planetology, School of Ocean and Earth Science and Technology, University of Hawaii, Honolulu HI 96822, USA. Present address: Central Oregon Community College, Bend OR 97702, USA. email@example.com
3 Geological Survey of Japan, 1-1-3 Higashi, Tsukuba, Ibaraki 305-8567, Japan.
receipt: 21 February 2000
Acceptance: 14 September 2000
Web publication: 16 April 2001