Ferromagnetic fraction of Cretaceous and Cenozoic sediments at DSDP Holes 72-515B and 72-516F

Fuente: PANGAEA
Salvato in:
Dettagli Bibliografici
Autori principali: Petrova, G N, Nechaeva, T B, Gurary, G Z, Chmerev, V A
Natura: Dataset Open Access
Lingua:en
Pubblicazione: PANGAEA 1983
Soggetti:
Accesso online:
Tags: Aggiungi Tag
Nessun Tag, puoi essere il primo ad aggiungerne!!
_version_ 1867168563184271360
author Petrova, G N
Nechaeva, T B
Gurary, G Z
Chmerev, V A
author_facet Petrova, G N
Nechaeva, T B
Gurary, G Z
Chmerev, V A
collection Datos científicos de ciencias marinas y ambientales
contents Investigation of the ferromagnetic fraction of sediments from the Brazil Basin and Rio Grande Rise shows that its main constituents are magnetite and hematite. The magnetite is detrital, but the hematite is both detrital and chemical in origin. Magnetite is the main carrier of the natural remanent magnetization (NRM); therefore, the NRM is detrital remanent magnetization (DRM). In a number of cases, the change of magnetic parameters along the stratigraphic column permits some refinement of the previously defined boundaries of the lithologic units.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_811470
institution PANGAEA
language en
publishDate 1983
publisher PANGAEA
record_format pangaea
spellingShingle Ferromagnetic fraction of Cretaceous and Cenozoic sediments at DSDP Holes 72-515B and 72-516F
Petrova, G N
Nechaeva, T B
Gurary, G Z
Chmerev, V A
72-515B; 72-516F; Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; Glomar Challenger; Leg72; South Atlantic/BASIN; South Atlantic/CONT RISE
Investigation of the ferromagnetic fraction of sediments from the Brazil Basin and Rio Grande Rise shows that its main constituents are magnetite and hematite. The magnetite is detrital, but the hematite is both detrital and chemical in origin. Magnetite is the main carrier of the natural remanent magnetization (NRM); therefore, the NRM is detrital remanent magnetization (DRM). In a number of cases, the change of magnetic parameters along the stratigraphic column permits some refinement of the previously defined boundaries of the lithologic units.
title Ferromagnetic fraction of Cretaceous and Cenozoic sediments at DSDP Holes 72-515B and 72-516F
topic 72-515B; 72-516F; Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; Glomar Challenger; Leg72; South Atlantic/BASIN; South Atlantic/CONT RISE
url https://doi.org/10.1594/PANGAEA.811470