(Table 1) Components of magnetization at DSDP Hole 77-538A

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Autori principali: Testarmata, Margaret M, Gose, Wulf A
Natura: Dataset Open Access
Lingua:en
Pubblicazione: PANGAEA 1984
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_version_ 1867170029099810816
author Testarmata, Margaret M
Gose, Wulf A
author_facet Testarmata, Margaret M
Gose, Wulf A
collection Datos científicos de ciencias marinas y ambientales
contents At DSDP Sites 536 and 538 in the southeastern Gulf of Mexico, rocks from near the Cretaceous/Tertiary boundary were recovered. The Danian/Maestrichtian samples from Site 536 were stepwise demagnetized in alternating fields up to 400 Oe. Two distinct components of magnetization could be identified, neither of which displays a reversal pattern compatible with the age of the samples. Samples from the Danian section at Site 538 were subjected to a combination of alternating field and thermal demagnetization. Although several reversals are observed, a unique correlation with the magnetic time scale is not possible until the paleontology of the section is better defined.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_809677
institution PANGAEA
language en
publishDate 1984
publisher PANGAEA
record_format pangaea
spellingShingle (Table 1) Components of magnetization at DSDP Hole 77-538A
Testarmata, Margaret M
Gose, Wulf A
77-538A; Deep Sea Drilling Project; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Glomar Challenger; Gulf of Mexico/KNOLL; Leg77; MAG; Magnetometer; NRM, Declination; NRM, Inclination; Sample code/label
At DSDP Sites 536 and 538 in the southeastern Gulf of Mexico, rocks from near the Cretaceous/Tertiary boundary were recovered. The Danian/Maestrichtian samples from Site 536 were stepwise demagnetized in alternating fields up to 400 Oe. Two distinct components of magnetization could be identified, neither of which displays a reversal pattern compatible with the age of the samples. Samples from the Danian section at Site 538 were subjected to a combination of alternating field and thermal demagnetization. Although several reversals are observed, a unique correlation with the magnetic time scale is not possible until the paleontology of the section is better defined.
title (Table 1) Components of magnetization at DSDP Hole 77-538A
topic 77-538A; Deep Sea Drilling Project; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Glomar Challenger; Gulf of Mexico/KNOLL; Leg77; MAG; Magnetometer; NRM, Declination; NRM, Inclination; Sample code/label
url https://doi.org/10.1594/PANGAEA.809677