"Pumpellyit vznikl v d\u016Fsledku p\u0159\u00EDzniv\u00E9ho zdrojov\u00E9ho materi\u00E1lu, anchimetamorfn\u00EDch podm\u00EDnek a retrogr\u00E1dn\u00EDch reakc\u00ED, spojen\u00FDch s fluidn\u00EDm p\u0159\u00EDnosem. Jeho p\u0159\u00EDtomnost roz\u0161i\u0159uje spektrum miner\u00E1l\u016F v topografick\u00E9 mineralogii Moravy. Anchimetamorfn\u00ED podm\u00EDnky p\u0159ibli\u017Ene odpov\u00EDdaj\u00ED prehnit-pumpellyitov\u00E9 subfacii. Pozdn\u011B syn- a\u017E postkinematick\u00E1 mikrostrukturn\u00ED poz\u00EDce a dal\u0161\u00ED krit\u00E9ria indikuj\u00ED, \u017Ee pumpellyit vznikal v procesu chladnut\u00ED, n\u00E1sledn\u011B po rann\u011B permsk\u00E9m granitov\u00E9m magmatismu." . . . "\u017D\u00E1\u010Dek, Vladim\u00EDr" . "Pumpellyite formed due to favourable source material, anchimetamorphic condition and retrogressive reactions, connected with fluid input. Its existence extends the mineral spectrum of topographic mineralogy in the Movavian part in the Moravian rock-units. Metamorphic conditions are constrained at sub-greenschist facies, roughly conforming to the prehnite-pumpellyite subfacies. Late syn- to postkinematic microtextural position and other criteria indicate that origin of pumpellyite was induced by cooling processes succeeding the Early Permian granitic magmatism."@en . . "Geologick\u00E9 v\u00FDzkumy na Morav\u011B a ve Slezsku" . "CZ - \u010Cesk\u00E1 republika" . "283488" . . "RIV/00025798:_____/10:00000394!RIV11-MZP-00025798" . . "RIV/00025798:_____/10:00000394" . . "pumpellyite, Jesen\u00EDk amphibolite massif, Silesicum, Bohemian Massif"@en . . "Kov\u00E1\u010Dik, Martin" . "Pecina, Vratislav" . "Pumpellyit \u2013 miner\u00E1l z\u00E1v\u011Bre\u010Dn\u00E9 metamorfn\u00ED f\u00E1ze v bytownitov\u00E9 rule vrbensk\u00E9 skupiny a v amfibolitu jesenick\u00E9ho mas\u00EDvu (silezikum)" . "Pumpellyit \u2013 miner\u00E1l z\u00E1v\u011Bre\u010Dn\u00E9 metamorfn\u00ED f\u00E1ze v bytownitov\u00E9 rule vrbensk\u00E9 skupiny a v amfibolitu jesenick\u00E9ho mas\u00EDvu (silezikum)"@cs . . . . "17" . "4"^^ . "zima" . "I, Z(MZP0002579801)" . "5"^^ . "Pumpellyite \u2013 product of late metamorphic phase from bytownite gneiss of Vrbno Group and amphibolite of Jesen\u00EDk massif (Silesicum, Bohemian massif)"@en . . . . "1212-6209" . . . "Pumpellyit \u2013 miner\u00E1l z\u00E1v\u011Bre\u010Dn\u00E9 metamorfn\u00ED f\u00E1ze v bytownitov\u00E9 rule vrbensk\u00E9 skupiny a v amfibolitu jesenick\u00E9ho mas\u00EDvu (silezikum)"@cs . "3"^^ . . "Opletal, Mojm\u00EDr" . "Pumpellyite \u2013 product of late metamorphic phase from bytownite gneiss of Vrbno Group and amphibolite of Jesen\u00EDk massif (Silesicum, Bohemian massif)"@en . "[FA74763FB3E9]" . "Pumpellyit vznikl v d\u016Fsledku p\u0159\u00EDzniv\u00E9ho zdrojov\u00E9ho materi\u00E1lu, anchimetamorfn\u00EDch podm\u00EDnek a retrogr\u00E1dn\u00EDch reakc\u00ED, spojen\u00FDch s fluidn\u00EDm p\u0159\u00EDnosem. Jeho p\u0159\u00EDtomnost roz\u0161i\u0159uje spektrum miner\u00E1l\u016F v topografick\u00E9 mineralogii Moravy. Anchimetamorfn\u00ED podm\u00EDnky p\u0159ibli\u017Ene odpov\u00EDdaj\u00ED prehnit-pumpellyitov\u00E9 subfacii. Pozdn\u011B syn- a\u017E postkinematick\u00E1 mikrostrukturn\u00ED poz\u00EDce a dal\u0161\u00ED krit\u00E9ria indikuj\u00ED, \u017Ee pumpellyit vznikal v procesu chladnut\u00ED, n\u00E1sledn\u011B po rann\u011B permsk\u00E9m granitov\u00E9m magmatismu."@cs . . . "Pumpellyit \u2013 miner\u00E1l z\u00E1v\u011Bre\u010Dn\u00E9 metamorfn\u00ED f\u00E1ze v bytownitov\u00E9 rule vrbensk\u00E9 skupiny a v amfibolitu jesenick\u00E9ho mas\u00EDvu (silezikum)" . .