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| Main Authors: | , |
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| Format: | Dataset Open Access |
| Language: | en |
| Published: |
PANGAEA
1982
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| Online Access: | https://doi.org/10.1594/PANGAEA.817078 |
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| _version_ | 1867169083773943808 |
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| author | Hailwood, Ernie A Rees, A I |
| author_facet | Hailwood, Ernie A Rees, A I |
| collection | Datos científicos de ciencias marinas y ambientales |
| contents | Measurements were made of the magnetic properties of 13 sediment samples from cores spanning the entire depth of Hole 503A. The principal aim was to make a preliminary assessment of the magnetic fabric of material obtained from hydraulic piston coring (HPC) which, though considerably bioturbated, might retain substantial traces of any depositional alignment of magnetic grains. Earlier measurements on Deep Sea Drilling Project cores (Rees, 1971; Rees and Frederick, 1974; Hailwood and Sayre, 1979) suggested that the improved HPC sampling technique should, other things being equal, provide good magnetic fabric information. The Hole 503A sediments were known from shipboard measurements to possess comparatively strong stable remanence and therefore seemed likely subjects for this assessment. |
| format | Dataset Open Access |
| id | pangaea_https___doi_org_10_1594_PANGAEA_817078 |
| institution | PANGAEA |
| language | en |
| publishDate | 1982 |
| publisher | PANGAEA |
| record_format | pangaea |
| spellingShingle | (Table 1) Magnetic properties of specimens from DSDP Hole 68-503A Hailwood, Ernie A Rees, A I 68-503A; Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Glomar Challenger; Koenigsberger ratio; Leg68; MAG; Magnetometer; North Pacific/FLANK; NRM, Intensity; NRM, Intensity after demagnetization; Parameter; Sample code/label; Susceptibility Measurements were made of the magnetic properties of 13 sediment samples from cores spanning the entire depth of Hole 503A. The principal aim was to make a preliminary assessment of the magnetic fabric of material obtained from hydraulic piston coring (HPC) which, though considerably bioturbated, might retain substantial traces of any depositional alignment of magnetic grains. Earlier measurements on Deep Sea Drilling Project cores (Rees, 1971; Rees and Frederick, 1974; Hailwood and Sayre, 1979) suggested that the improved HPC sampling technique should, other things being equal, provide good magnetic fabric information. The Hole 503A sediments were known from shipboard measurements to possess comparatively strong stable remanence and therefore seemed likely subjects for this assessment. |
| title | (Table 1) Magnetic properties of specimens from DSDP Hole 68-503A |
| topic | 68-503A; Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Glomar Challenger; Koenigsberger ratio; Leg68; MAG; Magnetometer; North Pacific/FLANK; NRM, Intensity; NRM, Intensity after demagnetization; Parameter; Sample code/label; Susceptibility |
| url | https://doi.org/10.1594/PANGAEA.817078 |