(Dobrá Voda)
Granitic lepidolite pegmatite in Strážek Moldanubicum. Symetracilly zoned steeply dipping dyke up to 6 m thick and about 100 m long in amphibolite and gneiss. Known since 1934.
NOTE: Not to be confused with the Dobrá Voda locality in Bohemia (Ag-(Au)-polymetallic mineralization).
Refs.:
Novák, M., Staněk, J.: Lepidolitový pegmatit od Dobré Vody u Velkého Meziříčí, západní Morava. Acta Musei Moraviae, Scientiae geologicae, 1999, roč. 84, s. 3 - 44.
Ercit, T.S., Černý, P., Hawthorne, F.C. (1993) Cesstibtantite: a geologic introduction to the inverse pyrochlores. Mineralogy and Petrology: 48: 235-255;
Novak & Srein (1998) Niobian cesstibtantite from Dobra Voda lepidolite pegmatite, western Moravia, Czech Republic. Neues Jahrbuch Miner., Mh. 354-360.
- Canadian Mineralogist Vol. 38, pp. 1399-1408 (2000)
Mineral List:36 entries listed. 29 valid minerals.
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