"1"^^ . . . "1"^^ . "0514-8057" . "I" . "podzim" . "5"^^ . "Kambrium u Slapnick\u00E9ho ml\u00FDna a Jez\u00EDrek a nov\u00FD v\u00FDskyt sediment\u016F kambria v\u00FDchodn\u011B od Mle\u010Dic" . "Neuveden" . . . . . "RIV/00025798:_____/13:00000248!RIV14-MSM-00025798" . "Kambrium u Slapnick\u00E9ho ml\u00FDna a Jez\u00EDrek a nov\u00FD v\u00FDskyt sediment\u016F kambria v\u00FDchodn\u011B od Mle\u010Dic"@cs . . "Cambrian near Slapnick\u00FD ml\u00FDn and Jez\u00EDrka localities and new occurrence of Cambrian sediments eastward from Mle\u010Dice village"@en . "Vorel, Tom\u00E1\u0161" . . . . . "[74274D25A075]" . "Geological mapping on the sheet Podmokly has supplemented the knowledge on some classical localities in Skryje-T\u00FD\u0159ovice Cambrian (Slapnick\u00FD ml\u00FDn, Jez\u00EDrka and Mle\u010Dice) by new findings. At the locality of Slapnick\u00FD ml\u00FDn two new tectonically affected outcrops of Mile\u010D conglomerates are described at the left-hand side of the Zbiro\u017Esk\u00FD potok valley. These two outcrops are tectonically separated from the occurence of Mile\u010D conglomerates in the gorge above the Slapnice camp. Above this camp the conglomerates already show its correct, tectonically unaffected position and NE\u2013SW course. Coarse siliceous conglomerates, developed in the upper part of Mile\u010D Conglomerates in this area, probably correspond to the former rocky coast facie. At the locality of Jez\u00EDrka, about 250 metres from the waterfall, the lamprophyre intrusion, formerly considered to be a tectonic fault, is newly described. The vein has an E\u2013W course and is significantly altered (calcified). East of Mle\u010Dice village, in a deeply cut gorge, a new occurrence of Cambrian sediments (shales and siltstones) is described. The Cambrian is exposed there at the bottom of a narrow stream, in a section about 500\u2013700 metres eastwards from the center of Mle\u010Dice village. It is probably a tectonically restricted segment of sediments inside andesites of the K\u0159ivokl\u00E1t-Rokycany Volcanic Complex. On earlier maps this occurrence has never been reported."@en . "Geologick\u00FDm mapov\u00E1n\u00EDm na listu Podmokly byly n\u011Bkter\u00E9 klasick\u00E9 lokality ve skryjsko-t\u00FD\u0159ovick\u00E9m kambriu (Slapnick\u00FD ml\u00FDn, Jez\u00EDrka a Mle\u010Dice) dopln\u011Bny o nov\u00E9 poznatky. Na lokalit\u011B Slapnick\u00FD ml\u00FDn byly pops\u00E1ny dva nov\u00E9, tektonicky posti\u017Een\u00E9 v\u00FDchozy mile\u010Dsk\u00FDch slepenc\u016F v prav\u00E9 \u010D\u00E1sti \u00FAdol\u00ED Zbiro\u017Esk\u00E9ho potoka. Tektonicky jsou odd\u011Bleny od v\u00FDchoz\u016F mile\u010Dsk\u00FDch slepenc\u016F v rokli nad kempem Slapnice. Zde maj\u00ED slepence ji\u017E stratigraficky spr\u00E1vnou, tektonicky neovlivn\u011Bnou polohu a JZ-SV pr\u016Fb\u011Bh. Hrub\u00FD buli\u017En\u00EDkov\u00FD slepenec, zachovan\u00FD ve svrchn\u00ED \u010D\u00E1sti mile\u010Dsk\u00FDch slepenc\u016F v t\u00E9to oblasti, p\u0159edstavuje patrn\u011B tehdej\u0161\u00ED p\u0159\u00EDbojovou facii. Na lokalit\u011B Jez\u00EDrka, cca 250 m s. od vodop\u00E1du, byla pops\u00E1na intruze lamprofyru, pokl\u00E1dan\u00E1 d\u0159\u00EDve za zlom. \u017D\u00EDla m\u00E1 Z\u2013V pr\u016Fb\u011Bh a je v\u00FDrazn\u011B alterovan\u00E1 (kalcifikovan\u00E1). V\u00FDchodn\u011B od Mle\u010Dic, v hluboce za\u0159\u00EDzl\u00E9 rokli, byl pops\u00E1n nov\u00FD v\u00FDskyt kambrick\u00FDch sediment\u016F (b\u0159idlic a prachovc\u016F). Kambrium zde vych\u00E1z\u00ED jen ve dn\u011B pot\u016F\u010Dku, zhruba v \u00FAseku 500 a\u017E 700 m v. od centra Mle\u010Dic. Jde patrn\u011B o tektonicky omezenou kru uvnit\u0159 andezit\u016F k\u0159ivokl\u00E1tsko-rokycansk\u00E9ho komplexu. Na star\u0161\u00EDch map\u00E1ch nen\u00ED tento v\u00FDskyt uv\u00E1d\u011Bn." . "RIV/00025798:_____/13:00000248" . "Zpr\u00E1vy o geologick\u00FDch v\u00FDzkumech v roce 2012" . "CZ - \u010Cesk\u00E1 republika" . "82317" . . "Geologick\u00FDm mapov\u00E1n\u00EDm na listu Podmokly byly n\u011Bkter\u00E9 klasick\u00E9 lokality ve skryjsko-t\u00FD\u0159ovick\u00E9m kambriu (Slapnick\u00FD ml\u00FDn, Jez\u00EDrka a Mle\u010Dice) dopln\u011Bny o nov\u00E9 poznatky. Na lokalit\u011B Slapnick\u00FD ml\u00FDn byly pops\u00E1ny dva nov\u00E9, tektonicky posti\u017Een\u00E9 v\u00FDchozy mile\u010Dsk\u00FDch slepenc\u016F v prav\u00E9 \u010D\u00E1sti \u00FAdol\u00ED Zbiro\u017Esk\u00E9ho potoka. Tektonicky jsou odd\u011Bleny od v\u00FDchoz\u016F mile\u010Dsk\u00FDch slepenc\u016F v rokli nad kempem Slapnice. Zde maj\u00ED slepence ji\u017E stratigraficky spr\u00E1vnou, tektonicky neovlivn\u011Bnou polohu a JZ-SV pr\u016Fb\u011Bh. Hrub\u00FD buli\u017En\u00EDkov\u00FD slepenec, zachovan\u00FD ve svrchn\u00ED \u010D\u00E1sti mile\u010Dsk\u00FDch slepenc\u016F v t\u00E9to oblasti, p\u0159edstavuje patrn\u011B tehdej\u0161\u00ED p\u0159\u00EDbojovou facii. Na lokalit\u011B Jez\u00EDrka, cca 250 m s. od vodop\u00E1du, byla pops\u00E1na intruze lamprofyru, pokl\u00E1dan\u00E1 d\u0159\u00EDve za zlom. \u017D\u00EDla m\u00E1 Z\u2013V pr\u016Fb\u011Bh a je v\u00FDrazn\u011B alterovan\u00E1 (kalcifikovan\u00E1). V\u00FDchodn\u011B od Mle\u010Dic, v hluboce za\u0159\u00EDzl\u00E9 rokli, byl pops\u00E1n nov\u00FD v\u00FDskyt kambrick\u00FDch sediment\u016F (b\u0159idlic a prachovc\u016F). Kambrium zde vych\u00E1z\u00ED jen ve dn\u011B pot\u016F\u010Dku, zhruba v \u00FAseku 500 a\u017E 700 m v. od centra Mle\u010Dic. Jde patrn\u011B o tektonicky omezenou kru uvnit\u0159 andezit\u016F k\u0159ivokl\u00E1tsko-rokycansk\u00E9ho komplexu. Na star\u0161\u00EDch map\u00E1ch nen\u00ED tento v\u00FDskyt uv\u00E1d\u011Bn."@cs . "Cambrian, Skryje-T\u00FD\u0159ovice Basin, Buchava Formation, stratigraphy, tectonics, lamprophyres, geological mapping"@en . . "Cambrian near Slapnick\u00FD ml\u00FDn and Jez\u00EDrka localities and new occurrence of Cambrian sediments eastward from Mle\u010Dice village"@en . "Kambrium u Slapnick\u00E9ho ml\u00FDna a Jez\u00EDrek a nov\u00FD v\u00FDskyt sediment\u016F kambria v\u00FDchodn\u011B od Mle\u010Dic" . . . . . . . "Kambrium u Slapnick\u00E9ho ml\u00FDna a Jez\u00EDrek a nov\u00FD v\u00FDskyt sediment\u016F kambria v\u00FDchodn\u011B od Mle\u010Dic"@cs .