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Autori principali: Keating, Barbara, Sakai, Hideo
Natura: Dataset Open Access
Lingua:en
Pubblicazione: PANGAEA 1991
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Accesso online:https://doi.org/10.1594/PANGAEA.758523
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author Keating, Barbara
Sakai, Hideo
author_facet Keating, Barbara
Sakai, Hideo
collection Datos científicos de ciencias marinas y ambientales
contents Paleomagnetic studies conducted on board JOIDES Resolution during Leg 119 indicate that the cores collected at Site 744 range from Quaternary through Eocene in age. Initial studies of the sediments completed on board the ship measured the magnetization of the archive halves of the sedimentary cores, using the pass-through cryogenic magnetometer. Stratigraphic plots of the declination and inclination derived from these measurements displayed numerous long intervals with essentially constant magnetic directions. Further study of these intervals led to a discovery that the background signal had been incorrectly computed due to faulty software on the ship. Because this background signal was not recorded in the data-processing system, corrections could not be made. Therefore, subsequent shorebased studies have been made on the individual samples collected at approximately 30-cm intervals in the cores in order to verify the initial magnetostratigraphy reported in the Initial Reports volume for Leg 119 (Barron, Larsen, et al., 1989, doi:10.2973/odp.proc.ir.119.1989). Numerous reversals were identified and correlations were suggested with the seafloor magnetic anomaly sequence of Berggren et al. (1985, doi:10.1130/0016-7606(1985)96<1407:CG>2.0.CO;2) back to anomaly number 17.
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institution PANGAEA
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publishDate 1991
publisher PANGAEA
record_format pangaea
spellingShingle Paleomagnetic properties of ODP Site 119-744 (Appendix)
Keating, Barbara
Sakai, Hideo
119-744A; 119-744B; Demagnetization level; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Event label; Indian Ocean; Joides Resolution; Leg119; NRM, Declination after demagnetization; NRM, Inclination after demagnetization; NRM, Intensity after demagnetization; Ocean Drilling Program; ODP; Polarity; Sample code/label
Paleomagnetic studies conducted on board JOIDES Resolution during Leg 119 indicate that the cores collected at Site 744 range from Quaternary through Eocene in age. Initial studies of the sediments completed on board the ship measured the magnetization of the archive halves of the sedimentary cores, using the pass-through cryogenic magnetometer. Stratigraphic plots of the declination and inclination derived from these measurements displayed numerous long intervals with essentially constant magnetic directions. Further study of these intervals led to a discovery that the background signal had been incorrectly computed due to faulty software on the ship. Because this background signal was not recorded in the data-processing system, corrections could not be made. Therefore, subsequent shorebased studies have been made on the individual samples collected at approximately 30-cm intervals in the cores in order to verify the initial magnetostratigraphy reported in the Initial Reports volume for Leg 119 (Barron, Larsen, et al., 1989, doi:10.2973/odp.proc.ir.119.1989). Numerous reversals were identified and correlations were suggested with the seafloor magnetic anomaly sequence of Berggren et al. (1985, doi:10.1130/0016-7606(1985)96<1407:CG>2.0.CO;2) back to anomaly number 17.
title Paleomagnetic properties of ODP Site 119-744 (Appendix)
topic 119-744A; 119-744B; Demagnetization level; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Event label; Indian Ocean; Joides Resolution; Leg119; NRM, Declination after demagnetization; NRM, Inclination after demagnetization; NRM, Intensity after demagnetization; Ocean Drilling Program; ODP; Polarity; Sample code/label
url https://doi.org/10.1594/PANGAEA.758523