(Table T1) Magnetic anisotropy of samples from ODP Hole 180-1117A
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| Format: | Dataset Open Access |
| Sprache: | en |
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PANGAEA
2001
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| _version_ | 1867172320254099456 |
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| author | Ishikawa, Naoto Frost, Gina Marie |
| author_facet | Ishikawa, Naoto Frost, Gina Marie |
| collection | Datos científicos de ciencias marinas y ambientales |
| contents | At Site 1117, drilled during Leg 180 of the Ocean Drilling Program in the Woodlark Basin, we cored a fault zone and recovered fault gouge, mylonitized and brecciated gabbros, and undeformed gabbro. We measured the anisotropy of magnetic susceptibility for the rock samples. The susceptibilities of the fault gouge samples were lower than those of the undeformed gabbro, and those of deformed gabbros were lowest. The anisotropy degrees of the fault gouge samples were higher than those of the deformed and undeformed gabbros. Oblate magnetic fabrics were dominant in the samples from the fault zone. |
| format | Dataset Open Access |
| id | pangaea_https___doi_org_10_1594_PANGAEA_787082 |
| institution | PANGAEA |
| language | en |
| publishDate | 2001 |
| publisher | PANGAEA |
| record_format | pangaea |
| spellingShingle | (Table T1) Magnetic anisotropy of samples from ODP Hole 180-1117A Ishikawa, Naoto Frost, Gina Marie 180-1117A; Declination of principle axis K1; Declination of principle axis K2; Declination of principle axis K3; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Inclination of principle axis K1; Inclination of principle axis K2; Inclination of principle axis K3; Joides Resolution; Leg180; Magnetic susceptibility, volume; Magnitude of anisotropy; Ocean Drilling Program; ODP; Piece; Principle axes K1 of normalized anisotropy tensor; Principle axes K2 of normalized anisotropy tensor; Principle axes K3 of normalized anisotropy tensor; Sample code/label; Sample comment; Shape of susceptibility; Solomon Sea; Susceptibility unit Kappabridge KLY-2; Volume At Site 1117, drilled during Leg 180 of the Ocean Drilling Program in the Woodlark Basin, we cored a fault zone and recovered fault gouge, mylonitized and brecciated gabbros, and undeformed gabbro. We measured the anisotropy of magnetic susceptibility for the rock samples. The susceptibilities of the fault gouge samples were lower than those of the undeformed gabbro, and those of deformed gabbros were lowest. The anisotropy degrees of the fault gouge samples were higher than those of the deformed and undeformed gabbros. Oblate magnetic fabrics were dominant in the samples from the fault zone. |
| title | (Table T1) Magnetic anisotropy of samples from ODP Hole 180-1117A |
| topic | 180-1117A; Declination of principle axis K1; Declination of principle axis K2; Declination of principle axis K3; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Inclination of principle axis K1; Inclination of principle axis K2; Inclination of principle axis K3; Joides Resolution; Leg180; Magnetic susceptibility, volume; Magnitude of anisotropy; Ocean Drilling Program; ODP; Piece; Principle axes K1 of normalized anisotropy tensor; Principle axes K2 of normalized anisotropy tensor; Principle axes K3 of normalized anisotropy tensor; Sample code/label; Sample comment; Shape of susceptibility; Solomon Sea; Susceptibility unit Kappabridge KLY-2; Volume |
| url | https://doi.org/10.1594/PANGAEA.787082 |