"83-922218-4-2" . "Western Carpathians, Carpathian foredeep, boreholes, lower Paleozoic clastics, mineralogical and chemical composition"@en . "Z(MZP0002579801)" . . . "The Lower Palaeozoic clastic sediments are the non-metamorphic siliciclastic sediments forming the platform sedimentary cover of Brunovistulicum and underlying the Moravian platform carbonates. Twelve samples of basal clastic sediments were collected from the boreholes: M\u011Bn\u00EDn-1, N\u011Bm\u010Di\u010Dky-6; Kory\u010Dany-3, Mile\u0161ovice-1, Nikol\u010Dice-4, Slavkov-2, \u0160v\u00E1benice-1, T\u011B\u0161any-1, Uh\u0159ice-6, \u017Dd\u00E1nice-14. The siliciclastic sediments display different lithology. They include conglomerates, sandstones and mudstones. Generally the mineralogically mature sandstones prevail over arcoses and arcosic sandstones. The ultra-stable translucent heavy minerals (zircon, rutile and tourmaline) usually dominate, apatite and garnet are often present. Hornblende, pyroxene, staurolite, epidote group, kyanite, chromite, sphene and monazite were found in accessoric amounts." . "Study of heavy minerals in the Lower Palaeozoic clastic sediments found in boreholes (SE Moravia, Czech Republic)"@en . "Krakow" . . . "Study of heavy minerals in the Lower Palaeozoic clastic sediments found in boreholes (SE Moravia, Czech Republic)" . "Materialy konferencyjne. Streszczenia referat\u00F3w i poster\u00F3w." . "[6ED5810F56F6]" . . . . . . "Study of heavy minerals in the Lower Palaeozoic clastic sediments found in boreholes (SE Moravia, Czech Republic)"@en . "4"^^ . . . "Study of heavy minerals in the Lower Palaeozoic clastic sediments found in boreholes (SE Moravia, Czech Republic)" . "Otava, Ji\u0159\u00ED" . "Z n\u011Bkter\u00FDch vrt\u016F (M\u011Bn\u00EDn-1, N\u011Bm\u010Di\u010Dky-6; Kory\u010Dany-3, Mile\u0161ovice-1, Nikol\u010Dice-4, Slavkov-2, \u0160v\u00E1benice-1, T\u011B\u0161any-1, Uh\u0159ice-6, \u017Dd\u00E1nice-14) dovrtan\u00FDch do spodnopaleozoick\u00FDch klastik byly z k\u0159emenn\u00FDch a\u017E ark\u00F3zov\u00FDch p\u00EDskovc\u016F odebr\u00E1ny vzorky na detailn\u011Bj\u0161\u00ED petrologick\u00E9 studium. Co se t\u00FD\u010De meneralogick\u00E9 skladby, tak ve v\u0161ech vzorc\u00EDch p\u0159eva\u017Euje asociace turmal\u00EDn, zirkon a rutil. Ojedin\u011Ble byl zji\u0161t\u011Bn apatit a gran\u00E1t a velmi vz\u00E1cn\u011B amfibol, pyroxen, epidot, kyanit, monazit."@cs . "2006-06-20+02:00"^^ . "4"^^ . "Studium t\u011B\u017Ek\u00FDch miner\u00E1l\u016F ve spodnopaleozoick\u00FDch sedimentech odebran\u00FDch z vrt\u016F (SV Morava, \u010Cesk\u00E1 republika)"@cs . "Gil\u00EDkov\u00E1, Helena" . "RIV/00025798:_____/06:00000097!RIV07-MZP-00025798" . . . . . "RIV/00025798:_____/06:00000097" . "Studium t\u011B\u017Ek\u00FDch miner\u00E1l\u016F ve spodnopaleozoick\u00FDch sedimentech odebran\u00FDch z vrt\u016F (SV Morava, \u010Cesk\u00E1 republika)"@cs . "Buri\u00E1nek, David" . "Leichmann, Jaroslav" . "Zwierzyniec" . . . "119" . "Uniwersytet Warszawski. Wydzia\u0142 Geologii. Instytut Geologii Podstawowej" . "1"^^ . "502262" . "The Lower Palaeozoic clastic sediments are the non-metamorphic siliciclastic sediments forming the platform sedimentary cover of Brunovistulicum and underlying the Moravian platform carbonates. Twelve samples of basal clastic sediments were collected from the boreholes: M\u011Bn\u00EDn-1, N\u011Bm\u010Di\u010Dky-6; Kory\u010Dany-3, Mile\u0161ovice-1, Nikol\u010Dice-4, Slavkov-2, \u0160v\u00E1benice-1, T\u011B\u0161any-1, Uh\u0159ice-6, \u017Dd\u00E1nice-14. The siliciclastic sediments display different lithology. They include conglomerates, sandstones and mudstones. Generally the mineralogically mature sandstones prevail over arcoses and arcosic sandstones. The ultra-stable translucent heavy minerals (zircon, rutile and tourmaline) usually dominate, apatite and garnet are often present. Hornblende, pyroxene, staurolite, epidote group, kyanite, chromite, sphene and monazite were found in accessoric amounts."@en . . . .