Inclination of the two main components of magnetization and 87Sr/86Sr ratios for dolomites at DSDP Hole 77-536

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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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author Testarmata, Margaret M
Gose, Wulf A
author_facet Testarmata, Margaret M
Gose, Wulf A
collection Datos científicos de ciencias marinas y ambientales
contents Site 536 terminated in a shallow-water dolomite of unknown age. Paleomagnetic measurements combined with strontium isotope analyses suggest that the dolomite was deposited in the Middle Jurassic to Early Cretaceous time interval. However, the assumptions required to reach this determination make these results less than conclusive.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_809676
institution PANGAEA
language en
publishDate 1984
publisher PANGAEA
record_format pangaea
spellingShingle Inclination of the two main components of magnetization and 87Sr/86Sr ratios for dolomites at DSDP Hole 77-536
Testarmata, Margaret M
Gose, Wulf A
77-536; Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; Glomar Challenger; Gulf of Mexico/SLOPE; Leg77
Site 536 terminated in a shallow-water dolomite of unknown age. Paleomagnetic measurements combined with strontium isotope analyses suggest that the dolomite was deposited in the Middle Jurassic to Early Cretaceous time interval. However, the assumptions required to reach this determination make these results less than conclusive.
title Inclination of the two main components of magnetization and 87Sr/86Sr ratios for dolomites at DSDP Hole 77-536
topic 77-536; Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; Glomar Challenger; Gulf of Mexico/SLOPE; Leg77
url https://doi.org/10.1594/PANGAEA.809676