The relationship between the magnetic anisotropy and the c-axis fabric in a massive hematite ore
Item
Title (Dublin Core)
en-US
The relationship between the magnetic anisotropy and the c-axis fabric in a massive hematite ore
Description (Dublin Core)
en-US
Preferred orientation of hematite ore from Minas Gerais, Brazil, was investigated by reflected-light microscopy, X-ray structural goniometry and magnetic anisotropy. A close relationship was found between c-axis fabrics determined by magnetic and non-magnetic methods; experiments confirmed the results of the theoretical treatment. For routine work it is advantageous to use both types of methods, profiting from rapidity of measurement of magnetic anisotropy and from detailed c-axis pole figures of pilot specimens provided by X-ray goniometry.
ARK: https://n2t.net/ark:/88439/y048352
Permalink: https://geophysicsjournal.com/article/244
ARK: https://n2t.net/ark:/88439/y048352
Permalink: https://geophysicsjournal.com/article/244
Creator (Dublin Core)
Hrouda, F.
Siemes, H.
Herres, N.
Hennig-Michaeli, C.
Subject (Dublin Core)
en-US
Hematite ore
en-US
c-axis fabric
en-US
Magnetic anisotropy
en-US
Solid Earth
Publisher (Dublin Core)
en-US
Journal of Geophysics
Date (Dublin Core)
1984-12-13
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/244
Source (Dublin Core)
en-US
Journal of Geophysics; Vol 56 No 1 (1985): Journal of Geophysics; 174-182
2643-2986
2643-9271
Language (Dublin Core)
eng
Relation (Dublin Core)
https://journal.geophysicsjournal.com/JofG/article/view/244/204