. "Mineral and textural evolution of a subvolcanic A-type granite: Hora Svat\u00E9 Kate\u0159iny stock, Kru\u0161n\u00E9 Hory Mts., Czech Republic" . . . "Zeitschrift f\u00FCr geologische Wissenschaften" . "RIV/67985831:_____/08:00325626" . . . "Kate\u0159inohorsk\u00FD granit tvo\u0159\u00ED pe\u0148 o pr\u016Fm\u011Bru asi 100 m 2 km z\u00E1p. od Hora svat\u00E9 Kate\u0159iny. Intrudoval ve dvou pulsech: 1. st\u0159edn\u011B zrnit\u00FD neporfyrick\u00FD biotitick\u00FD granit tvo\u0159\u00ED p\u0159ev\u00E1\u017Enou \u010D\u00E1st pn\u011B, a 2. jemnozrnn\u00FD \u0159\u00EDdce drobn\u011B porfyrick\u00FD leukogranit. Chemick\u00E1 charakteristika granit\u016F odpov\u00EDd\u00E1 A-typu taveniny: granity jsou jen nepatrn\u011B peraluminick\u00E9 (ASI=1.05), obohacen\u00E9 o fluor (kolem 0.5 % F), Rb (900-1200 ppm), Nb (60-80 ppm), Ta (10-15 ppm), Th (30-50 ppm), Zr (100-160 ppm), Y (74-157 ppm) a Be (5-19 ppm.), a ochuzen\u00E9 fosforem (0.1 wt% P2O5). Oba granity obsahuj\u00ED krystaly pertitu v z\u00E1kladn\u00ED hmot\u011B slo\u017Een\u00E9 z k\u0159emene, K-\u017Eivce, albitu a Li-annitu. B\u011B\u017En\u00FDmi magmatick\u00FDmi akcesoriemi jsou fluorit, magnetit a zirkon. V men\u0161\u00EDm mno\u017Estv\u00ED je p\u0159\u00EDtomen topaz, beryl, xenotim, monazit, thorit, kasiterit, kolumbit a dal\u0161\u00ED Nb,Ta,U-f\u00E1ze. \u010Cernovit, rhapdophan, bastn\u00E4sit a Ce- oxyfluoridy jsou spolu s Fe-oxidy and hydroxidy produkty intenzivn\u00ED hydroterm\u00E1ln\u00ED alterace.P\u0159ibli\u017En\u00E9 st\u00E1\u0159\u00ED granitu je 310+- 14 Ma."@cs . "A-type granite; rock textures; mineralogy; geochemistry; Kru\u0161n\u00E9 Hory Mts.; Erzgebirge"@en . . "Miner\u00E1ln\u00ED a texturn\u00ED v\u00FDvoj subvulkanick\u00E9ho slab\u011B peraluminick\u00E9ho granitu z Hory svat\u00E9 Kate\u0159iny (\u010Cesk\u00E1 republika)"@cs . . "36" . . "Mineral and textural evolution of a subvolcanic A-type granite: Hora Svat\u00E9 Kate\u0159iny stock, Kru\u0161n\u00E9 Hory Mts., Czech Republic" . "DE - Spolkov\u00E1 republika N\u011Bmecko" . . "RIV/67985831:_____/08:00325626!RIV09-AV0-67985831" . "Breiter, Karel" . . "6" . "1"^^ . . "379509" . . "0303-4534" . "P(IAA300130801), Z(AV0Z30130516)" . "Mineral and textural evolution of a subvolcanic A-type granite: Hora Svat\u00E9 Kate\u0159iny stock, Kru\u0161n\u00E9 Hory Mts., Czech Republic"@en . "Mineral and textural evolution of a subvolcanic A-type granite: Hora Svat\u00E9 Kate\u0159iny stock, Kru\u0161n\u00E9 Hory Mts., Czech Republic"@en . . "18"^^ . "1"^^ . . "The Hora Svat\u00E9 Kate\u0159iny granite forms a small stock in the Kru\u0161n\u00E9 Hory / Erzgebirge Mts. Granite emplacement proceeded in two pulses: (i) Equigranular medium-grained biotite granite; (ii) Fine-porphyritic fine-grained leucogranite. Chemical features correspond to an A-type character of the granite. Rock is slightly peraluminous (ASI=1.05), rich in fluorine (about 0.5 wt% F), Rb (about 900-1200 ppm), Nb (60-80 ppm), Ta (10-15 ppm), Th (30-50 ppm), Zr (100-160 ppm), Y (74-157 ppm) and Be (5-19 ppm.), and poor in P (0.1 wt% P2O5). Both granite types contain phenocrysts of perthitic K-feldspar in groundmass composed of quartz, K-feldspar, albite and Li-bearing annite. Magmatic accessory phases comprise fluorite, magnetite, zircon, topaz, beryl, xenotime, monazite, thorite, cassiterite, and columbite. Chernovite, rhabdophane, bastn\u00E4site, and Ce-dominated oxyfluoride are products of intensive hydrothermal alteration. The Th-U-total Pb age of monazite yielded the age of 308 +- 14 Ma."@en . "Miner\u00E1ln\u00ED a texturn\u00ED v\u00FDvoj subvulkanick\u00E9ho slab\u011B peraluminick\u00E9ho granitu z Hory svat\u00E9 Kate\u0159iny (\u010Cesk\u00E1 republika)"@cs . . . . . . "The Hora Svat\u00E9 Kate\u0159iny granite forms a small stock in the Kru\u0161n\u00E9 Hory / Erzgebirge Mts. Granite emplacement proceeded in two pulses: (i) Equigranular medium-grained biotite granite; (ii) Fine-porphyritic fine-grained leucogranite. Chemical features correspond to an A-type character of the granite. Rock is slightly peraluminous (ASI=1.05), rich in fluorine (about 0.5 wt% F), Rb (about 900-1200 ppm), Nb (60-80 ppm), Ta (10-15 ppm), Th (30-50 ppm), Zr (100-160 ppm), Y (74-157 ppm) and Be (5-19 ppm.), and poor in P (0.1 wt% P2O5). Both granite types contain phenocrysts of perthitic K-feldspar in groundmass composed of quartz, K-feldspar, albite and Li-bearing annite. Magmatic accessory phases comprise fluorite, magnetite, zircon, topaz, beryl, xenotime, monazite, thorite, cassiterite, and columbite. Chernovite, rhabdophane, bastn\u00E4site, and Ce-dominated oxyfluoride are products of intensive hydrothermal alteration. The Th-U-total Pb age of monazite yielded the age of 308 +- 14 Ma." . "[FDF3CCD6E060]" . .