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Index Geophysics

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
 

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