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(Table T1) Anisotropy of magnetic susceptibility of ODP Hole 174B-1074A
To reveal compaction processes and mechanisms, we have studied microtextures and magnetic fabrics of unlithified sediments collected from Hole 1074A, on the eastern flank of the... -
(Table 1) Anisotropy of magnetic susceptibility parameters of ODP Hole 134-833B
Ocean Drilling Program (ODP) Sites 832 and 833 were drilled in the intra-arc North Aoba Basin of the New Hebrides Island Arc (Vanuatu). High volcanic influxes in the intra-arc... -
(Table 1) Magnetic susceptibility from IODP Hole 308-U1322B
The continental slope of the northern Gulf of Mexico seaward of the Mississippi Delta is characterized by very rapid Quaternary sedimentation. Thick sequences of... -
Anisotropy-magnetic susceptibility from IODP Hole 322-C0011B
Geocode = [m CSF-A] Top Core depth (below sea floor) -
Anisotropy-magnetic susceptibility from IODP Hole 322-C0012A
Geocode = [m CSF-A] Top Core depth (below sea floor) -
Anisotropy-magnetic susceptibility from IODP Hole 316-C0006E
Geocode = [m CSF-A] Top Core depth (below sea floor) -
Anisotropy-magnetic susceptibility from IODP Hole 316-C0004C
Geocode = [m CSF-A] Top Core depth (below sea floor) -
Anisotropy-magnetic susceptibility from IODP Hole 316-C0004D
Geocode = [m CSF-A] Top Core depth (below sea floor) -
Anisotropy-magnetic susceptibility from IODP Hole 319-C0009A
Geocode = [m CSF-A] Top Core depth (below sea floor) -
(Table 1) Anisotropy of magnetic susceptibility and paleomagnetic results for...
The fabric of fine-grained sediments from the deep-sea terrace on the landward side of the Japan Trench, cored during Ocean Drilling Program Leg 186, was analyzed using the...
