NRM intensity, MDF, stable inclination and susceptibility of cement samples of ODP Hole 109-648B (Table 1)
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| Autori principali: | , |
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| Natura: | Dataset Open Access |
| Lingua: | en |
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PANGAEA
1990
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| _version_ | 1867169977709101056 |
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| author | Hamano, Yozo Ohno, Masao |
| author_facet | Hamano, Yozo Ohno, Masao |
| collection | Datos científicos de ciencias marinas y ambientales |
| contents | The remanence properties of 62 cement samples from Cores 7R, 11R, and 12R recovered from Hole 648B were examined. The remanent magnetization consists of two components, where the soft component is carried by the basalt fragments in the cement sample and the hard component is carried by fine magnetic grains originally contained in cement. The hard component was used to estimate the variation of the magnetic field inclination within the hole. The result indicates that some parts of the basalt section within the sub-bottom depth between 15 and 20 m are reversely magnetized, which can be attributed to the displacement of pillow basalt after its solidification. |
| format | Dataset Open Access |
| id | pangaea_https___doi_org_10_1594_PANGAEA_745566 |
| institution | PANGAEA |
| language | en |
| publishDate | 1990 |
| publisher | PANGAEA |
| record_format | pangaea |
| spellingShingle | NRM intensity, MDF, stable inclination and susceptibility of cement samples of ODP Hole 109-648B (Table 1) Hamano, Yozo Ohno, Masao 109-648B; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Joides Resolution; Leg109; North Atlantic Ocean; NRM, Inclination; NRM, Intensity; NRM, Median destructive field of natural remanent magnetization; Ocean Drilling Program; ODP; Sample code/label; Susceptibility The remanence properties of 62 cement samples from Cores 7R, 11R, and 12R recovered from Hole 648B were examined. The remanent magnetization consists of two components, where the soft component is carried by the basalt fragments in the cement sample and the hard component is carried by fine magnetic grains originally contained in cement. The hard component was used to estimate the variation of the magnetic field inclination within the hole. The result indicates that some parts of the basalt section within the sub-bottom depth between 15 and 20 m are reversely magnetized, which can be attributed to the displacement of pillow basalt after its solidification. |
| title | NRM intensity, MDF, stable inclination and susceptibility of cement samples of ODP Hole 109-648B (Table 1) |
| topic | 109-648B; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Joides Resolution; Leg109; North Atlantic Ocean; NRM, Inclination; NRM, Intensity; NRM, Median destructive field of natural remanent magnetization; Ocean Drilling Program; ODP; Sample code/label; Susceptibility |
| url | https://doi.org/10.1594/PANGAEA.745566 |