. "sk"@cs . "Apulskou"@cs . . "1047679"^^ . "5342639"^^ . . . . . . . . "16369864"^^ . . "Adriatick\u00E9/Apulsk\u00E9"@cs . . . . . . "Apulsk\u00E9 mikrodesky"@cs . . "Jadersk\u00E1 deska"@cs . . . . . . "Jadersk\u00E1 deska"@cs . . . . "Jadersk\u00E1 nebo Apulsk\u00E1 deska je mal\u00E1 tektonick\u00E1 deska tvo\u0159en\u00E1 p\u0159ev\u00E1\u017En\u011B kontinent\u00E1ln\u00ED zemskou k\u016Frou, kter\u00E1 se odd\u011Blila od Africk\u00E9 desky, resp. Gondwany pod\u00E9l velk\u00E9ho sm\u011Brn\u00E9ho posunu b\u011Bhem k\u0159\u00EDdy. Ozna\u010Den\u00ED jadersk\u00E1 (adriatick\u00E1) deska se b\u011B\u017En\u011B pou\u017E\u00EDv\u00E1 pro jej\u00ED severn\u00ED \u010D\u00E1st, kter\u00E1 byla deformovan\u00E1 b\u011Bhem alpinsk\u00E9 Orogeneze, v jej\u00EDm\u017E pr\u016Fb\u011Bhu narazila na euroasijskou desku. Suturou po t\u00E9to sr\u00E1\u017Ece je Periadriatick\u00E1 linie, kter\u00E1 tvo\u0159\u00ED osu Alp. Apulsk\u00E1 deska se dodnes pohybuje v\u016F\u010Di Evropsk\u00E9 plotn\u011B pom\u011Brn\u011B nez\u00E1visle.Deska tvo\u0159\u00ED velkou \u010D\u00E1st Apeninsk\u00E9ho poloostrova a jej\u00ED \u010D\u00E1st je tak\u00E9 zalita Jadersk\u00FDm mo\u0159em. Hrub\u00E9 souvrstv\u00ED druhohorn\u00EDch v\u00E1penc\u016F usazen\u00FDch na jej\u00EDm povrchu formuj\u00ED ji\u017En\u00ED v\u00E1pencov\u00E9 Alpy. Na mnoha generalizovan\u00FDch paelogegrafick\u00FDch map\u00E1ch zab\u00EDr\u00E1 oblast It\u00E1lie, \u0158ecka, Balk\u00E1nu, Panonsk\u00E9 p\u00E1nve a Vnit\u0159n\u00EDch Z\u00E1padn\u00EDch Karpat, ale mikroplat\u0148a zahrnuj\u00EDc\u00ED Alpy, Karpaty a Panonii se naz\u00FDv\u00E1 Alcapa.Jadersk\u00E1 deska s sebou p\u016Fvodn\u011B nesla i \u010D\u00E1sti oce\u00E1nsk\u00E9 k\u016Fry piemontsk\u00FDch-Ligursk\u00E9ho oce\u00E1nu, kter\u00FD ji odd\u011Bloval od Brian\u00E7onnaisk\u00E9ho mikrokontinentu. Tento oce\u00E1n v\u0161ak v pr\u016Fb\u011Bhu k\u0159\u00EDdy subdukoval. V tomto obdob\u00ED narazila na euroasijsk\u00FDch desku v\u00FDchodn\u00ED a severn\u00ED \u010D\u00E1st Apulsk\u00E9 plotny. Tento proces trval do eoc\u00E9nu, n\u00E1sledn\u011B b\u011Bhem eoc\u00E9nu a mioc\u00E9nu tento pokra\u010Dovala sr\u00E1\u017Eka v z\u00E1padn\u00ED \u010D\u00E1sti. Z\u00E1kladn\u00ED modelov\u00E9 situace podle teorie deskov\u00E9 tektoniky obvykle ignoruj\u00ED mo\u017Enost subduk\u010Dn\u00ED kontinent\u00E1ln\u00ED k\u016Fry. N\u011Bkolik pozorov\u00E1n\u00ED v\u0161ak nasv\u011Bd\u010Duj\u00ED, \u017Ee v n\u011Bkter\u00FDch p\u0159\u00EDpadech k podobn\u00E9mu jevu v p\u0159\u00EDrod\u011B m\u016F\u017Ee doj\u00EDt. Pokud je kontinent\u00E1ln\u00ED k\u016Fra ten\u010D\u00ED ne\u017E 20 km, jej\u00ED hustota je srovnateln\u00E1 nebo dokonce v\u011Bt\u0161\u00ED ne\u017E v astenosf\u00E9ra a proto m\u016F\u017Ee subdukova\u0165. N\u011Bkolik geofyzik\u00E1ln\u00ED v\u00FDpo\u010Dty v Z\u00E1padn\u00EDch Alp\u00E1ch poukazuj\u00ED na to, \u017Ee k podobn\u00E9mu jevu muselo doj\u00EDt i p\u0159i koliz\u00ED Apulsk\u00E1 desky s Evropskou deskou, jej\u00ED\u017E hmoty byly \u010D\u00E1ste\u010Dn\u011B pohlceno pod Apulsk\u00E1 plotnou.Z jihu pod Apulsk\u00E1 plotnou subdukuje oce\u00E1nsk\u00E1 k\u016Fra Africk\u00E9 desky, jde o zbytky druhohor oce\u00E1nu Tethys. K tomuto doch\u00E1z\u00ED hlavn\u011B na z\u00E1pad\u011B a jihu Apeninsk\u00E9ho poloostrova. P\u0159i procesu tak\u00E9 doch\u00E1z\u00ED k hromad\u011Bn\u00ED sediment\u016F, kter\u00E9 jsou utr\u017Een\u00E9 z oce\u00E1nsk\u00E9ho dna, vznikaj\u00ED tzv. subduk\u010Dn\u00ED melan\u017Ee. Subduk\u010Dn\u00ED a n\u00E1sledn\u011B natavov\u00E1n\u00ED pohlcen\u00E9 oce\u00E1nsk\u00E9 k\u016Fry m\u00E1 za n\u00E1sledek vulkanismus v ji\u017En\u00EDm It\u00E1lii."@cs . . "Apulsk\u00E9 desky"@cs . . . . . "Apulsk\u00E1 plat\u0148a"@cs . "Jadersk\u00E1 nebo Apulsk\u00E1 deska je mal\u00E1 tektonick\u00E1 deska tvo\u0159en\u00E1 p\u0159ev\u00E1\u017En\u011B kontinent\u00E1ln\u00ED zemskou k\u016Frou, kter\u00E1 se odd\u011Blila od Africk\u00E9 desky, resp. Gondwany pod\u00E9l velk\u00E9ho sm\u011Brn\u00E9ho posunu b\u011Bhem k\u0159\u00EDdy. Ozna\u010Den\u00ED jadersk\u00E1 (adriatick\u00E1) deska se b\u011B\u017En\u011B pou\u017E\u00EDv\u00E1 pro jej\u00ED severn\u00ED \u010D\u00E1st, kter\u00E1 byla deformovan\u00E1 b\u011Bhem alpinsk\u00E9 Orogeneze, v jej\u00EDm\u017E pr\u016Fb\u011Bhu narazila na euroasijskou desku. Suturou po t\u00E9to sr\u00E1\u017Ece je Periadriatick\u00E1 linie, kter\u00E1 tvo\u0159\u00ED osu Alp."@cs . . . . . "42"^^ . . . . . "jadersk\u00E9 desky"@cs . . . . . . . . "4214"^^ . . "Apulsk\u00E9"@cs . .