(Table 1) Remanence properties of samples from ODP Core 126-792A-7H

Fuente: PANGAEA
Salvato in:
Dettagli Bibliografici
Autori principali: Cisowski, Stanley M, Koyama, Masato
Natura: Dataset Open Access
Lingua:en
Pubblicazione: PANGAEA 1992
Soggetti:
Accesso online:
Tags: Aggiungi Tag
Nessun Tag, puoi essere il primo ad aggiungerne!!
_version_ 1867170917765873664
author Cisowski, Stanley M
Koyama, Masato
author_facet Cisowski, Stanley M
Koyama, Masato
collection Datos científicos de ciencias marinas y ambientales
contents A combination of high sedimentation rates and high concentrations of magnetic grains in cores from Ocean Drilling Program Leg 126 resulted in the recovery of detailed direction and intensity records of the Brunhes/Matuyama geomagnetic polarity reversal. Virtual geomagnetic poles (VGPs) computed from azimuthally oriented samples taken from the cores of Hole 792A in the western Izu-Bonin forearc basin reveal that the geomagnetic pole persisted at moderate to high southern latitudes for several thousand years before a rapid migration to northern latitudes. Alternating-field demagnetization behavior, as well as NRM, NRM/ARM, and NRM/IRM intensities for samples from this same interval, and the NRM/IRM intensities derived from unoriented core samples from Holes 790C and 791B, drilled in the ~100-km distant Sumisu Rift, all suggest that the dipole field oscillated widely in intensity before the reversal. The fast polarity change occurred at the low point of an ~1100-yr field intensity cycle. This "reversal cycle" immediately followed earlier intensity cycles whose peaks rivaled or surpassed the normalized intensities of discrete samples from well above and below the reversal interval; furthermore, the troughs indicate a much diminished dipole field at their nadir.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_773510
institution PANGAEA
language en
publishDate 1992
publisher PANGAEA
record_format pangaea
spellingShingle (Table 1) Remanence properties of samples from ODP Core 126-792A-7H
Cisowski, Stanley M
Koyama, Masato
126-792A; ARM, Intensity, per unit volume; Demagnetization level; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; IRM, Intensity, per unit volume; Joides Resolution; Leg126; North Pacific Ocean; NRM, Intensity after demagnetization; NRM, Median destructive field/ARM, Median destructive field ratio; NRM, Median destructive field/IRM, Median destructive field ratio; Ocean Drilling Program; ODP; Sample code/label; Type; Virtual geomagnetic pole latitude; Virtual geomagnetic pole longitude
A combination of high sedimentation rates and high concentrations of magnetic grains in cores from Ocean Drilling Program Leg 126 resulted in the recovery of detailed direction and intensity records of the Brunhes/Matuyama geomagnetic polarity reversal. Virtual geomagnetic poles (VGPs) computed from azimuthally oriented samples taken from the cores of Hole 792A in the western Izu-Bonin forearc basin reveal that the geomagnetic pole persisted at moderate to high southern latitudes for several thousand years before a rapid migration to northern latitudes. Alternating-field demagnetization behavior, as well as NRM, NRM/ARM, and NRM/IRM intensities for samples from this same interval, and the NRM/IRM intensities derived from unoriented core samples from Holes 790C and 791B, drilled in the ~100-km distant Sumisu Rift, all suggest that the dipole field oscillated widely in intensity before the reversal. The fast polarity change occurred at the low point of an ~1100-yr field intensity cycle. This "reversal cycle" immediately followed earlier intensity cycles whose peaks rivaled or surpassed the normalized intensities of discrete samples from well above and below the reversal interval; furthermore, the troughs indicate a much diminished dipole field at their nadir.
title (Table 1) Remanence properties of samples from ODP Core 126-792A-7H
topic 126-792A; ARM, Intensity, per unit volume; Demagnetization level; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; IRM, Intensity, per unit volume; Joides Resolution; Leg126; North Pacific Ocean; NRM, Intensity after demagnetization; NRM, Median destructive field/ARM, Median destructive field ratio; NRM, Median destructive field/IRM, Median destructive field ratio; Ocean Drilling Program; ODP; Sample code/label; Type; Virtual geomagnetic pole latitude; Virtual geomagnetic pole longitude
url https://doi.org/10.1594/PANGAEA.773510