"Z(MSM 143100004)" . . . . "[0419AF2AB621]" . "CZ - \u010Cesk\u00E1 republika" . "Mineralogie a podm\u00EDnky vzniku \u010Dty\u0159 typ\u016F hydroterm\u00E1ln\u00ED mineralizace z lomu v Hrub\u00E9 Vod\u011B jsou klasifikov\u00E1ny do dvou z\u00E1kladn\u00EDch genetick\u00FDch kategori\u00ED a jsou prezentov\u00E1ny P-T charakteristiky hydroterm\u00E1ln\u00EDch proces\u016F."@cs . "Mineralogie a podm\u00EDnky vzniku \u010Dty\u0159 typ\u016F hydroterm\u00E1ln\u00ED mineralizace z lomu v Hrub\u00E9 Vod\u011B"@cs . "Slobodn\u00EDk, Marek" . "14310" . . . . . "4"^^ . . . "7-22" . "Mineralogy and formation conditions of the four types of hydrothermal mineralization from the quarry in Hrub\u00E1 Voda (Moravo-Silesian Culm)" . "RIV/00216224:14310/03:00009944!RIV/2005/MSM/143105/N" . . "Two main generation of hydrothermal veins have been distinquished, Variscan and post-Variscan. Genrations differ in mineral associations, type of fluids from which have been precipitated and in P-T formation conditions."@en . "Zim\u00E1k, Ji\u0159\u00ED" . "615591" . "1" . . . "3"^^ . "Doln\u00ED\u010Dek, Zden\u011Bk" . . "80-7067-566-7" . "Mineralogy and formation conditions of the four types of hydrothermal mineralization from the quarry in Hrub\u00E1 Voda (Moravo-Silesian Culm)"@en . "Mineralogie a podm\u00EDnky vzniku \u010Dty\u0159 typ\u016F hydroterm\u00E1ln\u00ED mineralizace z lomu v Hrub\u00E9 Vod\u011B"@cs . . . . "RIV/00216224:14310/03:00009944" . . "Culm; N\u00EDzk\u00FD Jesen\u00EDk; polymetallic veins; tectonics; fluid inclusions; stable isotopes; REE"@en . "Mal\u00FD, Karel" . . "38" . "Mineralogy and formation conditions of the four types of hydrothermal mineralization from the quarry in Hrub\u00E1 Voda (Moravo-Silesian Culm)" . . . "Acta Universitatis Palckianae Olomucensis, Geologica" . . "16"^^ . "Mineralogy and formation conditions of the four types of hydrothermal mineralization from the quarry in Hrub\u00E1 Voda (Moravo-Silesian Culm)"@en . "Two main generation of hydrothermal veins have been distinquished, Variscan and post-Variscan. Genrations differ in mineral associations, type of fluids from which have been precipitated and in P-T formation conditions." .