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Index Geophysics

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
 

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