Sediments from Sites 1057 and 1061 of Ocean Drilling Program Leg 172 on the Blake Outer Ridge exhibit nearly isotropic magnetic susceptibility. Resolving the degree of anisotropy of magnetic susceptibility proved difficult in many samples because of the generally weak magnetic susceptibility of the sediments relative to the noise level of the susceptibility meters used. Lineation varies from 1.0 to 1.013 and foliation varies from 1.0 to 1.08 in the samples that pass rejection criteria. In general the foliation is better resolved than the lineation, particularly at Site 1061, where the foliation exhibits long-term trends that mimic the mean susceptibility. The changes in the foliation at this site are likely the result of changes in the magn...
At Site 1117, drilled during Leg 180 of the Ocean Drilling Program in the Woodlark Basin, we cored a...
The fabric of fine-grained sediments from the deep-sea terrace on the landward side of the Japan Tre...
Susceptibility anisotropies in the form of vertically prolate ellipsoids have been reported in many ...
Paleomagnetic analysis of sediment samples from Ocean Drilling Program (ODP) Leg 133, Site 820, 10 k...
Due to the character of the original source materials and the nature of batch digitization, quality ...
The anisotropy of magnetic susceptibility (magnetic fabric) has been used as an aid to investigate t...
This study is a synthesis of paleomagnetic and mineral magnetic results for Sites 819 through 823 of...
Bulk magnetic susceptibility measurements on sedimentological samples from all geological periods ha...
Bulk magnetic susceptibility measurements on sedimentological samples from all geological periods ha...
Whole-core magnetic susceptibility measurements define a detailed stratigraphy that enables correlat...
The anisotropy of magnetic susceptibility documents the generation of tectonically produced fabrics ...
Shipboard magnetic investigation showed two zones of weak natural remanent magnetization (NRM): 675-...
Recognition of coring-induced disturbance, which is essential for magnetic fabric and paleomagnetic ...
Magnetic susceptibility (MS) measurements on carbonate rocks are considered as a proxy for impuritie...
Anisotropy of magnetic susceptibility data obtained from discrete subsamples recovered from two Inte...
At Site 1117, drilled during Leg 180 of the Ocean Drilling Program in the Woodlark Basin, we cored a...
The fabric of fine-grained sediments from the deep-sea terrace on the landward side of the Japan Tre...
Susceptibility anisotropies in the form of vertically prolate ellipsoids have been reported in many ...
Paleomagnetic analysis of sediment samples from Ocean Drilling Program (ODP) Leg 133, Site 820, 10 k...
Due to the character of the original source materials and the nature of batch digitization, quality ...
The anisotropy of magnetic susceptibility (magnetic fabric) has been used as an aid to investigate t...
This study is a synthesis of paleomagnetic and mineral magnetic results for Sites 819 through 823 of...
Bulk magnetic susceptibility measurements on sedimentological samples from all geological periods ha...
Bulk magnetic susceptibility measurements on sedimentological samples from all geological periods ha...
Whole-core magnetic susceptibility measurements define a detailed stratigraphy that enables correlat...
The anisotropy of magnetic susceptibility documents the generation of tectonically produced fabrics ...
Shipboard magnetic investigation showed two zones of weak natural remanent magnetization (NRM): 675-...
Recognition of coring-induced disturbance, which is essential for magnetic fabric and paleomagnetic ...
Magnetic susceptibility (MS) measurements on carbonate rocks are considered as a proxy for impuritie...
Anisotropy of magnetic susceptibility data obtained from discrete subsamples recovered from two Inte...
At Site 1117, drilled during Leg 180 of the Ocean Drilling Program in the Woodlark Basin, we cored a...
The fabric of fine-grained sediments from the deep-sea terrace on the landward side of the Japan Tre...
Susceptibility anisotropies in the form of vertically prolate ellipsoids have been reported in many ...