"Zeolite mineral assemblages from historical locality of Oslavany has been recently studied. Mineralization is developed on the fissures of amphibolite from the Svratka crystalline complex in the immediate contact of the Ole\u0161nice unit, Moravosilesian Zone. The most common zeolites are natrolite along with red-brown stilbite-Ca. Analcime occurs along with prehnite as pseudomorphs after laumontite. The most interesting mineral in the association is heulandite-K, a very rare end-member of heulandite series in the world known only from a few localities. This alpine paragenesis is characterized by a high content of Ca and was formed at low temperatures. High activity of K (heulandite-K) in the early stage and high activity of Na (analcime, natrolite) in the later stage are accompanied by overall high activity of Ca during the entire process."@en . . . "CZ - \u010Cesk\u00E1 republika" . "V" . "zeolite; natrolite; stilbite-Ca; analcime; heulandite-K; alpine veins; amphibolite; Oslavany; Czech Republic"@en . . "10"^^ . . . "Revize zeolit\u016F v alpsk\u00E9 paragenezi z historick\u00E9 lokality Oslavany (\u010Cesk\u00E1 republika)" . . "[1522DB70B0A0]" . . "Sejkora, Ji\u0159\u00ED" . "42660" . . "Revision of zeolites in Alpine paragenesis from the historical locality Oslavany (Czech Republic)"@en . . "3"^^ . . "Byla studov\u00E1na zeolitov\u00E1 miner\u00E1ln\u00ED asociace na historick\u00E9 lokalit\u011B Oslavany, kter\u00E1 je v\u00E1zan\u00E1 na trhliny amfibolit\u016F svrateck\u00E9ho krystalinika p\u0159i jeho kontaktu s ole\u0161nickou jednotkou moravika. V asociaci p\u0159evl\u00E1d\u00E1 natrolit nad \u010Dervenohn\u011Bd\u00FDm stilbitem-Ca, analcim s prehnitem tvo\u0159\u00ED pseudomorf\u00F3zy po laumontitu. Byl zji\u0161t\u011Bn heulandit-K, velmi vz\u00E1cn\u00FD i ve sv\u011Btov\u00E9m m\u011B\u0159\u00EDtku. Alpsk\u00E9 parageneze vznikla za n\u00EDzk\u00FDch teplot. V ran\u00E9m stadiu se nav\u00EDc uplatnila vysok\u00E1 aktivita K a pozd\u011Bji Na p\u0159i dominanci Ca b\u011Bhem cel\u00E9ho procesu."@cs . "Houzar, Stanislav" . "1211-0329" . "Revize zeolit\u016F v alpsk\u00E9 paragenezi z historick\u00E9 lokality Oslavany (\u010Cesk\u00E1 republika)"@cs . . . . . "Bulletin Mineralogicko-petrologick\u00E9ho odd\u011Blen\u00ED N\u00E1rodn\u00EDho muzea (Praha)" . "Revision of zeolites in Alpine paragenesis from the historical locality Oslavany (Czech Republic)"@en . . . "2"^^ . "Byla studov\u00E1na zeolitov\u00E1 miner\u00E1ln\u00ED asociace na historick\u00E9 lokalit\u011B Oslavany, kter\u00E1 je v\u00E1zan\u00E1 na trhliny amfibolit\u016F svrateck\u00E9ho krystalinika p\u0159i jeho kontaktu s ole\u0161nickou jednotkou moravika. V asociaci p\u0159evl\u00E1d\u00E1 natrolit nad \u010Dervenohn\u011Bd\u00FDm stilbitem-Ca, analcim s prehnitem tvo\u0159\u00ED pseudomorf\u00F3zy po laumontitu. Byl zji\u0161t\u011Bn heulandit-K, velmi vz\u00E1cn\u00FD i ve sv\u011Btov\u00E9m m\u011B\u0159\u00EDtku. Alpsk\u00E9 parageneze vznikla za n\u00EDzk\u00FDch teplot. V ran\u00E9m stadiu se nav\u00EDc uplatnila vysok\u00E1 aktivita K a pozd\u011Bji Na p\u0159i dominanci Ca b\u011Bhem cel\u00E9ho procesu." . . "Revize zeolit\u016F v alpsk\u00E9 paragenezi z historick\u00E9 lokality Oslavany (\u010Cesk\u00E1 republika)"@cs . "1" . "RIV/00094862:_____/14:#0001666" . "Toman, Ji\u0159\u00ED" . "Revize zeolit\u016F v alpsk\u00E9 paragenezi z historick\u00E9 lokality Oslavany (\u010Cesk\u00E1 republika)" . "22" . . "RIV/00094862:_____/14:#0001666!RIV15-MK0-00094862" . . . .