Rock magnetism of pelagic sediments from DSDP Leg 85 sites

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Main Authors: Worm, Horst-Ulrich, Weinreich, Norbert
Format: Dataset Open Access
Language:en
Published: PANGAEA 1988
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author Worm, Horst-Ulrich
Weinreich, Norbert
author_facet Worm, Horst-Ulrich
Weinreich, Norbert
collection Datos científicos de ciencias marinas y ambientales
contents A detailed rock magnetic investigation has been carried out on Deep Sea Drilling Project (DSDP) pelagic sediments from the Central Equatorial Pacific. This comprises hysteresis and thermomagnetic measurements, Lowrie-Fuller test and, for the first time, ferromagnetic resonance (FMR). Nearly stochiometric magnetite in two grain size fractions, single domain (SD) and multi domain (MD), has been deduced to be the carrier of magnetic remanence. Comparatively strong paramagnetic contributions are carried by pyrite, being identified by X-ray analysis. The statistical analysis of paleomagnetic parameters (NRM, MDF, initial susceptibility, Königsberger ratio Q) from a large number (> 1000) of samples, supported by hysteresis measurements, indicates a latitude and sedimentation rate dependent ratio of SD/MD grains. Possible sources for the magnetic constituents are discussed in terms of bacterial, volcanic, meteoritic and authigenic origin.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_725500
institution PANGAEA
language en
publishDate 1988
publisher PANGAEA
record_format pangaea
spellingShingle Rock magnetism of pelagic sediments from DSDP Leg 85 sites
Worm, Horst-Ulrich
Weinreich, Norbert
85-573; 85-574; 85-575; DRILL; Drilling/drill rig; Glomar Challenger; Leg85; North Pacific/FLANK; North Pacific/TROUGH; Ocean Drilling Program; ODP
A detailed rock magnetic investigation has been carried out on Deep Sea Drilling Project (DSDP) pelagic sediments from the Central Equatorial Pacific. This comprises hysteresis and thermomagnetic measurements, Lowrie-Fuller test and, for the first time, ferromagnetic resonance (FMR). Nearly stochiometric magnetite in two grain size fractions, single domain (SD) and multi domain (MD), has been deduced to be the carrier of magnetic remanence. Comparatively strong paramagnetic contributions are carried by pyrite, being identified by X-ray analysis. The statistical analysis of paleomagnetic parameters (NRM, MDF, initial susceptibility, Königsberger ratio Q) from a large number (> 1000) of samples, supported by hysteresis measurements, indicates a latitude and sedimentation rate dependent ratio of SD/MD grains. Possible sources for the magnetic constituents are discussed in terms of bacterial, volcanic, meteoritic and authigenic origin.
title Rock magnetism of pelagic sediments from DSDP Leg 85 sites
topic 85-573; 85-574; 85-575; DRILL; Drilling/drill rig; Glomar Challenger; Leg85; North Pacific/FLANK; North Pacific/TROUGH; Ocean Drilling Program; ODP
url https://doi.org/10.1594/PANGAEA.725500