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

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 s...

Full description

Bibliographic Details
Main Authors: Frost, Gina Marie, Yamazaki, Toshitsugu
Format: Dataset
Language:English
Published: PANGAEA 2001
Subjects:
175-1081C
ARM
Intensity after demagnetization
Benguela Current
South Atlantic Ocean
DEPTH
sediment/rock
DRILL
Drilling/drill rig
DSDP/ODP/IODP sample designation
IRM
Intensity
per unit volume
Joides Resolution
Kappabridge
Leg175
Magnetic susceptibility
volume
NRM
Ocean Drilling Program
ODP
Parameter
Sample code/label
Saturation isothermal remanent magnetisation
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.787570
https://doi.org/10.1594/PANGAEA.787570
Description
Summary: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.

Similar Items