"The Postojnska jama\u2013Planinska jama cave system and number of smaller caves between them are developed in the Postojnski kras situated between two dextral strike-slip fault zones of the Dinaric direction. Homogeneity of palaeomagnetic data can indicate fast deposition during short-lasted single-flood events. Such depositional style was favourable for record of short-lived excursions of the palaeomagnetic field. Most of studied sediments are younger than 0.78 Ma, some dates can indicate age deeply below 0.78 Ma. The cave system shows long evolution governed by the function of the Planinsko polje in the relation to the evolution of resurgence area in Ljubljana Moor farther on the east." . "Zupan-Hajna, N." . . "Cave sediments from the Postojnska-Planinska cave system (Slovenia): evidence of multi-phase evolution in epiphreatic zone"@en . . . . "Schnabl, Petr" . . "Cave sediments from the Postojnska-Planinska cave system (Slovenia): evidence of multi-phase evolution in epiphreatic zone" . . "dating; palaeomagnetism; magnetostratigraphy; karst geomorphology; Classical Karst"@en . "[3302F9BABEFF]" . "Pruner, Petr" . "358956" . "RIV/67985831:_____/08:00312825" . . "Cave sediments from the Postojnska-Planinska cave system (Slovenia): evidence of multi-phase evolution in epiphreatic zone" . "Acta carsologica" . "0583-6050" . . . . "Jeskynn\u00ED sedimenty syst\u00E9mu Postojnska-Planinska jama (Slovinsko): p\u0159\u00EDklad v\u00EDcef\u00E1zov\u00E9ho v\u00FDvoje v epifreatick\u00E9 z\u00F3n\u011B"@cs . "24"^^ . . "RIV/67985831:_____/08:00312825!RIV09-AV0-67985831" . "37" . . "3"^^ . . "1" . . . "SI - Slovinsk\u00E1 republika" . "Cave sediments from the Postojnska-Planinska cave system (Slovenia): evidence of multi-phase evolution in epiphreatic zone"@en . . "P(IAA300130701), Z(AV0Z30130516)" . . . "Mihevc, A." . "Jeskynn\u00ED sedimenty syst\u00E9mu Postojnska-Planinska jama (Slovinsko): p\u0159\u00EDklad v\u00EDcef\u00E1zov\u00E9ho v\u00FDvoje v epifreatick\u00E9 z\u00F3n\u011B"@cs . . . . "5"^^ . "The Postojnska jama\u2013Planinska jama cave system and number of smaller caves between them are developed in the Postojnski kras situated between two dextral strike-slip fault zones of the Dinaric direction. Homogeneity of palaeomagnetic data can indicate fast deposition during short-lasted single-flood events. Such depositional style was favourable for record of short-lived excursions of the palaeomagnetic field. Most of studied sediments are younger than 0.78 Ma, some dates can indicate age deeply below 0.78 Ma. The cave system shows long evolution governed by the function of the Planinsko polje in the relation to the evolution of resurgence area in Ljubljana Moor farther on the east."@en . "Syst\u00E9m Postojnska jama \u2013 Planinska jama a \u0159ada dal\u0161\u00EDch men\u0161\u00EDch jeskyn\u00ED je vyvinut v Postojensk\u00E9m krasu mezi dv\u011Bma z\u00F3nami pravostrann\u00FDch horizont\u00E1ln\u00EDch posun\u016F din\u00E1rsk\u00E9ho sm\u011Bru. Homogenita palomagnetick\u00FDch dat nazna\u010Duje, \u017Ee sedimenty mohou b\u00FDt v\u00FDsledkem rychl\u00E9 depozice b\u011Bhem kr\u00E1tk\u00FDch z\u00E1plavov\u00FDch ud\u00E1lost\u00ED. Tento styl ukl\u00E1d\u00E1n\u00ED byl p\u0159\u00EDzniv\u00FD pro z\u00E1znam kr\u00E1tkodob\u00FDch exkurz\u00ED paleomagnetick\u00E9ho pole. V\u011Bt\u0161ina studovan\u00FDch sediment\u016F je mlad\u0161\u00ED ne\u017E 0,78 Ma, n\u011Bkter\u00E1 z dat nazna\u010Duj\u00ED st\u00E1\u0159\u00ED hluboce pod 0,78 Ma. Jeskynn\u00ED syst\u00E9m se dlouhodob\u011B vyv\u00EDjel v n\u00E1vaznosti na funkci Planinsk\u00E9ho polje a v\u00FDvoji pramenn\u00E9 oblasti v Lubla\u0148sk\u00E9m baz\u00E9nu d\u00E1le na V."@cs . "Bos\u00E1k, Pavel" .