http://www.cnr.it/ontology/cnr/individuo/prodotto/ID187774
Tourmaline of the elbaite-dravite series from an elbaite-subtype pegmatite at Blizna, southern Bohemia, Czech Republic (Articolo in rivista)
- Type
- Label
- Tourmaline of the elbaite-dravite series from an elbaite-subtype pegmatite at Blizna, southern Bohemia, Czech Republic (Articolo in rivista) (literal)
- Anno
- 1999-01-01T00:00:00+01:00 (literal)
- Alternative label
Novak M. 1; Selway J.B. 2; Cerny P. 2; Hawthorne F.C. 2; Ottolini L. 3; (1999)
Tourmaline of the elbaite-dravite series from an elbaite-subtype pegmatite at Blizna, southern Bohemia, Czech Republic
in European journal of mineralogy (Print)
(literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#autori
- Novak M. 1; Selway J.B. 2; Cerny P. 2; Hawthorne F.C. 2; Ottolini L. 3; (literal)
- Pagina inizio
- Pagina fine
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#numeroVolume
- Rivista
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#numeroFascicolo
- Note
- ISI Web of Science (WOS) (literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#affiliazioni
- 1. Moravian Museum, Dept Mineral & Petrog, CZ-65937 Brno, Czech Republic;
2. Univ Manitoba, Dept Geol Sci, Winnipeg, MB R3T 2N2, Canada;
3. CNR, Ctr Studio Cristallochim & Cristallog, I-27100 Pavia, Italy; (literal)
- Titolo
- Tourmaline of the elbaite-dravite series from an elbaite-subtype pegmatite at Blizna, southern Bohemia, Czech Republic (literal)
- Abstract
- The elbaite-subtype pegmatite at Blizna, near Cerna v Posumavi in southern Bohemia, Czech Republic, intrudes dolomite-calcite marble. It can be divided into two distinct units, unit A and unit B, and has a narrow exocontact zone along the edge of the pegmatite. The crystallization sequence of tourmaline from unit A is Ca-rich schorl-elbaite --> Ca-rich elbaite-schorl-dravite --> Mn-rich elbaite --> Mn-rich liddicoatite --> liddicoatite-elbaite, typical of tourmaline from elbaite-subtype pegmatites. The crystallization sequence of tourmaline from unit B is Na-rich uvite --> Ca-rich schorl-elbaite-dravite --> Ca-rich Mg-bearing elbaite --> (Ca, Mn)-rich elbaite --> Mn-rich liddicoatite-elbaite --> Na-rich liddicoatite. Tourmaline from the exocontact ranges from Na-rich uvite --> Ca-rich dravite --> dravite-elbaite --> Ca-rich Mg-bearing elbaite --> liddicoatite-elbaite. The intermediate elbaite-schorl-dravite from unit A and schorl-elbaite-dravite from unit B are characterized by low F, moderate Mn and high Ti and Ca contents. The Mg-bearing elbaite from unit B and the exocontact is characterized by low Fe, moderate Ti, and high Ca and F contents. The dravite-elbaite from the exocontact is characterized by low Fe, Mn, Ti, Ca and F contents. The intermediate elbaite-schorl-dravite and elbaite-dravite solid-solutions crystallized as a result of mixing of (Ca, Mg)-rich fluids from the dolomite-calcite marble host-rock and exsolved (Na, Al, Li, F, B)-rich pegmatitic fluids. The factors controlling formation of elbaite-dravite in rocks may be summarized as follows: high activities of Li, Mg, Al and B, high Li/Mg ratio in the parent medium, acidic conditions with pHacidic conditions with pH
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