Pseudo-single-domain effects and single-domain multidomain transition in natural pyrrhotite deduced from domain structure observations
Item
Title (Dublin Core)
en-US
Pseudo-single-domain effects and single-domain multidomain transition in natural pyrrhotite deduced from domain structure observations
Description (Dublin Core)
en-US
The domain configuration of primary pyrrhotite in a Devonian diabase was studied using the Bitter pattern technique. Due to the uniaxial symmetry the multidomain grains have a rather simple domain structure. The single-domain — multidomain transition occurs at an average particle diameter of 1.6 μm. In the multidomain grains clusters of inclusions seem to produce pseudo-single-domain effects with complicated domain configurations. Such pseudo-single-domain effects are necessary for the interpretation of the magnetically hard component of remanence which cannot be explained by the observed abundance of true single-domain particles alone.
ARK: https://n2t.net/ark:/88439/y061450
Permalink: https://geophysicsjournal.com/article/91
ARK: https://n2t.net/ark:/88439/y061450
Permalink: https://geophysicsjournal.com/article/91
Creator (Dublin Core)
Soffel, H.
Subject (Dublin Core)
en-US
Rock magnetism
en-US
Domain structure
en-US
Pyrrhotite
en-US
Diabase
en-US
Palaeomagnetism
en-US
Experiment
Publisher (Dublin Core)
en-US
Journal of Geophysics
Date (Dublin Core)
1976-04-08
Type (Dublin Core)
info:eu-repo/semantics/article
info:eu-repo/semantics/publishedVersion
en-US
Peer-reviewed Article
Format (Dublin Core)
application/pdf
Identifier (Dublin Core)
https://journal.geophysicsjournal.com/JofG/article/view/91
Source (Dublin Core)
en-US
Journal of Geophysics; Vol 42 No 1 (1976): Journal of Geophysics; 351-359
2643-2986
2643-9271
Language (Dublin Core)
eng
Relation (Dublin Core)
https://journal.geophysicsjournal.com/JofG/article/view/91/52