"20"^^ . . "3555"^^ . "2007-01-01+01:00"^^ . "2"^^ . "Paleomagnetic research of karst sediments: paleotectonic and geomorfological implications"@en . "0"^^ . . "paleomagnetism; tectonics; magnetostratigraphy; biostratigraphy; dating; cave sediments; Europe"@en . "2011-12-31+01:00"^^ . . "Kras funguje jako past zachycuj\u00EDc\u00ED geologickou minulost. Krasov\u00E9 sedimenty (povrchov\u00E9 a jeskynn\u00ED) konzervuj\u00ED z\u00E1znam, kter\u00FD mimo kras m\u016F\u017Ee chyb\u011Bt. Jeskyn\u011B v\u011Bt\u0161inou obsahuj\u00ED z\u00E1znam posledn\u00EDho vypl\u0148ov\u00E1n\u00ED (fosilizace), ale v p\u0159\u00EDhodn\u00FDch podm\u00EDnk\u00E1ch zaznamen\u00E1vaj\u00ED v\u00EDce ud\u00E1lost\u00ED. S ohledem na polycykli\u010Dnost v\u00FDvoje v\u011Bt\u0161iny kras\u016F, krasov\u00E9 sedimenty mohou zachytit dlouh\u00E9 \u010Dasov\u00E9 \u00FAseky. Pou\u017Eit\u00ED \u0161irok\u00E9 \u0161k\u00E1ly geochronologick\u00FDch metod (magnetostratigrafie, magnetosusceptibilita, standardn\u00ED paleontologie a biostratigrafie, stabiln\u00ED izotopy, izotopov\u00E9 metody) tak m\u016F\u017Ee slou\u017Eit jako n\u00E1stroj pro pozn\u00E1n\u00ED kenozoick\u00E9 historie jednotliv\u00FDch krasov\u00FDch \u00FAzem\u00ED. Z\u00E1znam zachycen\u00FD v krasu obsahuje nejen data pro rozlu\u0161t\u011Bn\u00ED geomorfologick\u00E9ho v\u00FDvoje (speleogeneze, v\u00FDvoj reli\u00E9fu), ale rovn\u011B\u017E data pro rekonstrukci tektonick\u00FDch proces\u016F v mobiln\u00EDch oblastech. Krasov\u00E1 \u00FAzem\u00ED vhodn\u00E1 k vyu\u017Eit\u00ED tohoto typu rekonstrukc\u00ED byla pe\u010Dliv\u011B vybr\u00E1na (\u010CR, Slovensko, Polsko, Ma\u010Farsko, Slovinsko)."@cs . "Paleomagnetick\u00FD v\u00FDzkum krasov\u00FDch sediment\u016F: paleotektonick\u00E9 a geomorfologick\u00E9 vyu\u017Eit\u00ED"@cs . . . . . "Karst functions as trap of the geological past. Karst sediments (surface and cave) conserve unique records, which can miss outside the karstland. Caves mostly contain record of the last infilling (fossilisation) events, in favourable conditions record of more events. Resulting from polycyclicity of most of karsts, karst sediments can cover long time-spans. The application of broad variety of geochronologic methods (magnetostratigraphy, magnetosusceptibility stratigraphy, standard paleontology and biostratigraphy, stable isotopes, isotopic dating methods) can therefore represent a tool for the reconstruction of Cenozoic history in respective karst region. The karst record includes not only data for solution of geomorphic evolution itself (speleogenesis, karst landscape evolution), but also for reconstruction of tectonic events in mobile regions. Karst regions for the test of such kind of reconstructions were carefully selected (Czechia, Slovakia, Poland, Hungary, Slovenia)."@en . . . "3555"^^ . . "20"^^ . . "1"^^ .