"1" . . "The teschenite association located in southwest part the Silesian Unit of the flysh belt, the West Carpathians, consists of intrusive and extrusive igneous rocks with variable textures, structures and mineral abundances. These rocks comprise mainly basalt, monchiquite, fourchite, picrite, and teschenite. The results of the petrographical investigations provide evidence on their polyphase magmatic and postmagmatic evolution. Content Si, Al, Fe, K and Na grow in the melt during magmatic stages. The compositional evolution trend of pyroxene from Al-Ti diopside towards aegirine-augite and spinelides from chromium spinels core to magnetite rim can be explained due to crystallization of the residual melt under higher oxygen fugacity. The plenty of the observed textural and mineralogical features originated during injection of magma into wet sediments or extrusion on the sea floor and subsequent reaction with seawater. Alternation of pillow lavas, hyaloclastites, volcanoclastic rocks, sandstones and claystones was probably deposited in the bathyal zone, based on micropalaeontological and vulcanological evidence. During postmagmatic stage a part of the primary magmatic assemblage was transformed to the secondary minerals. Alteration products include chlorite, magnetite, serpentine, limonite, albite, titanite, K-fedspar and calcite, some of which fill vesicles and/or joints."@en . "2"^^ . . "139604" . . . . "[404C5004220D]" . "Studovan\u00E9 horniny tvo\u0159ily synsediment\u00E1rn\u00ED podmo\u0159sk\u00E9 v\u00FDlevy \u010Dasto prov\u00E1zen\u00E9 hyaloklastity a vulkanoklastick\u00FDmi horninami. N\u011Bkdy vulkanity intrudovaly do sediment\u016F v podob\u011B \u017Eil a drobn\u00FDch t\u011Bles. Velmi \u010Dasto tvo\u0159\u00ED vulkanick\u00FD materi\u00E1l p\u0159\u00EDm\u011Bs v okoln\u00EDch sedimentech (hlavn\u011B j\u00EDlovce a p\u00EDskovce). V\u011Bt\u0161ina vulkanoklastik a \u010D\u00E1st l\u00E1v m\u00E1 v\u00FDrazn\u00FD pod\u00EDl mandl\u00ED vypln\u011Bn\u00FDch sekund\u00E1rn\u00EDmi miner\u00E1ly. V\u00FDskyt dutin po plynech spolu s mikropaleontologickou interpretac\u00ED prost\u0159ed\u00ED potvrzuj\u00ED, \u017Ee k erupc\u00EDm doch\u00E1zelo v hlubokomo\u0159sk\u00E9 p\u00E1nvi nep\u0159esahuj\u00EDc\u00ED zat\u00EDm v\u00FDrazn\u011B hloubku okolo 1000 nebo 2000 m. \u0160lo tedy o p\u00E1nev charakteru Rud\u00E9ho mo\u0159e \u010Di St\u0159edozemn\u00EDho mo\u0159e, sp\u00ED\u0161e ne\u017E oce\u00E1nsk\u00E9 p\u00E1nve. Magma v\u011Bt\u0161iny hornin reagovalo s mo\u0159skou vodou b\u011Bhem sv\u00E9ho vm\u00EDst\u011Bn\u00ED do je\u0161t\u011B nezpevn\u011Bn\u00FDch sediment\u016F nebo p\u0159i v\u00FDlevu na mo\u0159sk\u00E9 dno. Tyto procesy v\u00FDrazn\u011B ovlivnily charakter erupc\u00ED. V d\u016Fsledku interakce magmatu s mo\u0159skou do\u0161lo na okraj\u00EDch t\u011Bles k rychl\u00E9mu schlazen\u00ED a dezintegraci horniny (vznik hyaloklastit\u016F). Interakce s vodu tak\u00E9 ovlivnila fugacitu kysl\u00EDku ve zbytkov\u00E9 tavenin\u011B. B\u011Bhem chladnut\u00ED l\u00E1v doch\u00E1zelo k sekund\u00E1rn\u00EDm p\u0159em\u011Bn\u00E1m v d\u016Fsledku interakce s okoln\u00ED mo\u0159skou nebo diagenetickou vodou a v\u011Bt\u0161ina vulkanick\u00E9ho skla spole\u010Dn\u011B s n\u011Bkter\u00FDmi miner\u00E1ly (oliv\u00EDn, plagioklas) podlehla intenzivn\u00ED alteraci. Vznikaly tak sekund\u00E1rn\u00ED ho\u0159\u010D\u00EDkem bohat\u00E9 miner\u00E1ly, jako jsou chlority a miner\u00E1ly serpentinov\u00E9 skupiny. Velmi \u010Dasto krystalizoval tak\u00E9 kalcit, kter\u00FD \u010D\u00E1ste\u010Dn\u011B zaplnil n\u011Bkter\u00E9 pseudomorf\u00F3zy po oliv\u00EDnu a pyroxenu. Nov\u00E9 v\u00FDzkumy potvrdily velk\u00FD vliv hydroterm\u00E1ln\u00ED alterace na miner\u00E1ln\u00ED asociaci studovan\u00FDch vulkanit\u016F. V\u011Bt\u0161ina vulkanick\u00FDch hornin skupiny monchiquit-pikrit obsahuje jen zbytky p\u016Fvodn\u00EDch magmatick\u00FDch miner\u00E1l\u016F. V d\u016Fsledku hydroterm\u00E1ln\u00EDch alterac\u00ED a zv\u011Btr\u00E1v\u00E1n\u00ED v n\u011Bkter\u00FDch p\u0159\u00EDpadech zcela zmizely magmatick\u00E9 miner\u00E1ly a hornina se zm\u011Bnila na sm\u011Bs j\u00EDlov\u00FDch miner\u00E1l\u016F, chlorit\u016F, k\u0159emene, albitu, zeolit\u016F a karbon\u00E1t\u016F." . "I" . "RIV/00025798:_____/12:00000237!RIV13-MSM-00025798" . "Horniny t\u011B\u0161\u00EDnitov\u00E9 asociace v okol\u00ED Vala\u0161sk\u00E9ho Mezi\u0159\u00ED\u010D\u00ED"@cs . . . . "Horniny t\u011B\u0161\u00EDnitov\u00E9 asociace v okol\u00ED Vala\u0161sk\u00E9ho Mezi\u0159\u00ED\u010D\u00ED" . . . "RIV/00025798:_____/12:00000237" . . . . . "Buri\u00E1nek, David" . "Studovan\u00E9 horniny tvo\u0159ily synsediment\u00E1rn\u00ED podmo\u0159sk\u00E9 v\u00FDlevy \u010Dasto prov\u00E1zen\u00E9 hyaloklastity a vulkanoklastick\u00FDmi horninami. N\u011Bkdy vulkanity intrudovaly do sediment\u016F v podob\u011B \u017Eil a drobn\u00FDch t\u011Bles. Velmi \u010Dasto tvo\u0159\u00ED vulkanick\u00FD materi\u00E1l p\u0159\u00EDm\u011Bs v okoln\u00EDch sedimentech (hlavn\u011B j\u00EDlovce a p\u00EDskovce). V\u011Bt\u0161ina vulkanoklastik a \u010D\u00E1st l\u00E1v m\u00E1 v\u00FDrazn\u00FD pod\u00EDl mandl\u00ED vypln\u011Bn\u00FDch sekund\u00E1rn\u00EDmi miner\u00E1ly. V\u00FDskyt dutin po plynech spolu s mikropaleontologickou interpretac\u00ED prost\u0159ed\u00ED potvrzuj\u00ED, \u017Ee k erupc\u00EDm doch\u00E1zelo v hlubokomo\u0159sk\u00E9 p\u00E1nvi nep\u0159esahuj\u00EDc\u00ED zat\u00EDm v\u00FDrazn\u011B hloubku okolo 1000 nebo 2000 m. \u0160lo tedy o p\u00E1nev charakteru Rud\u00E9ho mo\u0159e \u010Di St\u0159edozemn\u00EDho mo\u0159e, sp\u00ED\u0161e ne\u017E oce\u00E1nsk\u00E9 p\u00E1nve. Magma v\u011Bt\u0161iny hornin reagovalo s mo\u0159skou vodou b\u011Bhem sv\u00E9ho vm\u00EDst\u011Bn\u00ED do je\u0161t\u011B nezpevn\u011Bn\u00FDch sediment\u016F nebo p\u0159i v\u00FDlevu na mo\u0159sk\u00E9 dno. Tyto procesy v\u00FDrazn\u011B ovlivnily charakter erupc\u00ED. V d\u016Fsledku interakce magmatu s mo\u0159skou do\u0161lo na okraj\u00EDch t\u011Bles k rychl\u00E9mu schlazen\u00ED a dezintegraci horniny (vznik hyaloklastit\u016F). Interakce s vodu tak\u00E9 ovlivnila fugacitu kysl\u00EDku ve zbytkov\u00E9 tavenin\u011B. B\u011Bhem chladnut\u00ED l\u00E1v doch\u00E1zelo k sekund\u00E1rn\u00EDm p\u0159em\u011Bn\u00E1m v d\u016Fsledku interakce s okoln\u00ED mo\u0159skou nebo diagenetickou vodou a v\u011Bt\u0161ina vulkanick\u00E9ho skla spole\u010Dn\u011B s n\u011Bkter\u00FDmi miner\u00E1ly (oliv\u00EDn, plagioklas) podlehla intenzivn\u00ED alteraci. Vznikaly tak sekund\u00E1rn\u00ED ho\u0159\u010D\u00EDkem bohat\u00E9 miner\u00E1ly, jako jsou chlority a miner\u00E1ly serpentinov\u00E9 skupiny. Velmi \u010Dasto krystalizoval tak\u00E9 kalcit, kter\u00FD \u010D\u00E1ste\u010Dn\u011B zaplnil n\u011Bkter\u00E9 pseudomorf\u00F3zy po oliv\u00EDnu a pyroxenu. Nov\u00E9 v\u00FDzkumy potvrdily velk\u00FD vliv hydroterm\u00E1ln\u00ED alterace na miner\u00E1ln\u00ED asociaci studovan\u00FDch vulkanit\u016F. V\u011Bt\u0161ina vulkanick\u00FDch hornin skupiny monchiquit-pikrit obsahuje jen zbytky p\u016Fvodn\u00EDch magmatick\u00FDch miner\u00E1l\u016F. V d\u016Fsledku hydroterm\u00E1ln\u00EDch alterac\u00ED a zv\u011Btr\u00E1v\u00E1n\u00ED v n\u011Bkter\u00FDch p\u0159\u00EDpadech zcela zmizely magmatick\u00E9 miner\u00E1ly a hornina se zm\u011Bnila na sm\u011Bs j\u00EDlov\u00FDch miner\u00E1l\u016F, chlorit\u016F, k\u0159emene, albitu, zeolit\u016F a karbon\u00E1t\u016F."@cs . "Bub\u00EDk, Miroslav" . "CZ - \u010Cesk\u00E1 republika" . "97" . "Horniny t\u011B\u0161\u00EDnitov\u00E9 asociace v okol\u00ED Vala\u0161sk\u00E9ho Mezi\u0159\u00ED\u010D\u00ED"@cs . "Rocks of teschenite association in the surroundings of Vala\u0161sk\u00E9 Mezi\u0159\u00ED\u010D\u00ED"@en . "Rocks of teschenite association in the surroundings of Vala\u0161sk\u00E9 Mezi\u0159\u00ED\u010D\u00ED"@en . "1211-8796" . "Horniny t\u011B\u0161\u00EDnitov\u00E9 asociace v okol\u00ED Vala\u0161sk\u00E9ho Mezi\u0159\u00ED\u010D\u00ED" . . "22"^^ . "Acta Musei Moraviae, Scientae geologicae" . . "Silesian Unit, rocks of teschenite association, mineralogy, petrology"@en . . "2"^^ .