Beryl-columbitový pegmatit z Branné, Hrubý Jeseník
Článek v PDFActa Mus. Moraviae, Sci. Geol. 88 (2003), vydání 1–2, stránky 113-122
Článek
Abstrakt:
Beryl-columbite pegmatite from Branná, Hrubý Jesenik Mnts., Northern Moravia
Granitic pegmatite from Branná represents typical beryl-columbite pegmatite of the Hrubý Jeseník Mts. pegmatite field. Its internal structure, textural-paragenetic units and description of minerals are given.
Columbite-tantalite is a typical accessory mineral besides garnet and beryl. Dominant ferrocolumbite is enriched in Ti and Fe3+ relative to columbite-tantalite from other localities of this region.
Kontakt:
Milan Novák, Radek Škoda, Boris Urbánek, Institute of Geological Sciences, Masaryk University, Kotlářská 2, 61137 Brno, Czech Republic, e-mail: mnovak@sci.muni.cz, rskoda@sci.muni.cz, parisu@post.cz
Miroslav Nepejchal, Žižkova 8, 787 01 Šumperk, Czech Republic
Citace
Novák, M., Nepejchal, M., Škoda, R., Urbánek, B., 2003: Beryl-columbitový pegmatit z Branné, Hrubý Jeseník. – Acta Mus. Morav., Sci. Geol., 88, 1–2, 113–122 (with English summary)ISSN: 1211–8796