Titanite-ilmenite-magnetite phase relations in amphibolites of the Chýnov area (Bohemian Massif, Czech Republic)

Title:

Titanite-ilmenite-magnetite phase relations in amphibolites of the Chýnov area (Bohemian Massif, Czech Republic)

Creator:

Miloš René

Identifier:

https://cdk.lib.cas.cz/client/handle/uuid:17b2238d-e119-48de-96a9-87e796b99446
uuid:17b2238d-e119-48de-96a9-87e796b99446
issn:1214-9705

Subject:

Geologie. Meteorologie. Klimatologie, amfibolity, titanit, amphibolites, titanite, Česká vysočina (pohoří), Bohemian massif, Moldanubian Zone, ilmenite, magnetite, 7, and 551

Type:

article, články, model:article, and TEXT

Format:

print, bez média, and svazek

Description:

An assemblage of Al-bearing titanite, ilmenite and magnetite is present in polymetamorphic metabasite environment of the Varied group of the Moldanubian Zone. Titanite is characterized by coupled substitution (Al, Fe3+)+ (F, OH) - Ti + O, with a slight excess of (Al, Fe3+)-F component. Complex reaction rims of titanite around ilmenite occur in some cases. Ilmenites have FeTiO3 amounts usually above 96 mol.%, with some enrichment by MnTiO3 component (max. 8 mol.%). Magnetite has a negligible ulvöspinel component (max. 1 mol.%)., Miloš René., and Obsahuje bibliografii

Language:

English

Rights:

http://creativecommons.org/licenses/by-nc-sa/4.0/
policy:public

Source:

Acta geodynamica et geomaterialia : | 2008 Volume:5 | Number:3 (151)

Harvested from:

CDK

Metadata only:

false