"Brno" . "33;36" . . "Alkalicko-\u017Eivcov\u00E9 granity a p\u0159\u00EDbuzn\u00E9 granitick\u00E9 horniny jsou \u0161iroce roz\u0161\u00ED\u0159eny na \u00FAzem\u00ED v\u00FDchodn\u00EDho Mandalgovi v centr\u00E1ln\u00EDm Mongolsku. Pro tu praci byly zvoleny 4 alkalicko\u017Eivcov\u00E9 granitoidn\u00ED plutony mesozoick\u00E9ho st\u00E1\u0159\u00ED v okol\u00ED m\u011Bsa Mandalgovi. Alkalicko\u017Eivcov\u00E9 granitoidn\u00ED plutony mesozoick\u00E9ho st\u00E1\u0159\u00ED byly zvoleny \u00FAmysln\u011B jako reprezentativn\u00ED vzorek z mnoha mesozoick\u00FDch granitoidn\u00EDch pluton\u016F. Tyto granitoidn\u00ED horniny intrudovaly vr\u00E1mci Central Mongolian Igneous Belt (CMIB), kter\u00E1 se rozprost\u00EDr\u00E1 od v\u00FDchodu na z\u00E1pad v d\u00E9lce cca 1500 km. CMIB je hlavn\u00ED strukturn\u00ED zonou v\u00E1zanou na na intezivn\u00ED svchno paleozoickou tektonomagmatickou aktivitu kter\u00E1 byla pod\u0159\u00EDzena pohyb\u016Fm a odleh\u010Den\u00ED mikrokontinent\u016F a jejich zabudov\u00E1n\u00EDm do geologick\u00E9 stavby centr\u00E1ln\u00EDho a z\u00E1padn\u00EDho Mongolska p\u0159ev\u00E1\u017En\u011B v pr\u016Fb\u011Bhu spodn\u00EDho paleozoika. V n\u00E1sleduj\u00EDc\u00EDm obdob\u00ED zejm\u00E9na spodn\u00EDho mesozoika ale s projevy a\u017E do svrchn\u00EDho terc\u00E9ru byla magmatick\u00E1 aktivita soust\u0159ed\u011Bna v \u0161irok\u00E9 oblasti m\u00E9n\u011B stabilizovan\u00E9ho horninov\u00E9ho podlo\u017E\u00ED Mongolochotsk\u00E9ho p"@cs . . . . "Alkali feldspar granites and subordinate granitoid rocks are widely exposed in the eastern Mandalgobi of central Mongolia. These granitoids are emplaced in the area of the Central Mongolian Igneous Belt (CMIB), roughly extending across Mongolia for about 1500 kilometres from west to east with a latitudinal trend. The CMIB is a major structural zone characterized by intense late-Paleozoic tectono-magmatic activity partially superimposed on an ancient block or continental crust segment with evidence, at least in central and western Mongolia, of tectono magmatic events of late Rephean-early Paleozoic age and of middle Paleozoic age. In subsequent events from early Mesozoic up to late Tertiary magmatic activity including the emplacement of granitoid complexes developed periodically in the formerly (Permian) more to less stabilized setting. This activity took place over a very wide sector, extending east and north--eastwards from central Mongolia to the Pacific Ocean for some 2500 - 3000 km, thereby consti"@en . "Samec, Pavel" . "RIV/62156489:43410/05:00057976!RIV06-GA0-43410___" . "Kynick\u00FD, Jind\u0159ich" . . "RIV/62156489:43410/05:00057976" . . "2"^^ . . "4"^^ . "Alkalicko-\u017Eivcov\u00E9 granity; Mandal Gobi; Mongolsko; St\u0159edomongolsk\u00FD vyv\u0159elinov\u00FD p\u00E1s"@en . "Mendelova zem\u011Bd\u011Blsk\u00E1 a lesnick\u00E1 univerzita v Brn\u011B" . "Granitoids of the Central Mongolian Igneous Belt"@en . "43410" . . "Granitoids of the Central Mongolian Igneous Belt" . . . "Granitoids of the Central Mongolian Igneous Belt" . . . . "Hlavn\u00ED v\u00FDsledky pr\u016Fzkumu \u00FAzem\u00ED Mongolska v projektu Mongolsko 2000 -- 2005: shrnut\u00ED, hodnocen\u00ED a interpretace (I)" . "Alkali feldspar granites and subordinate granitoid rocks are widely exposed in the eastern Mandalgobi of central Mongolia. These granitoids are emplaced in the area of the Central Mongolian Igneous Belt (CMIB), roughly extending across Mongolia for about 1500 kilometres from west to east with a latitudinal trend. The CMIB is a major structural zone characterized by intense late-Paleozoic tectono-magmatic activity partially superimposed on an ancient block or continental crust segment with evidence, at least in central and western Mongolia, of tectono magmatic events of late Rephean-early Paleozoic age and of middle Paleozoic age. In subsequent events from early Mesozoic up to late Tertiary magmatic activity including the emplacement of granitoid complexes developed periodically in the formerly (Permian) more to less stabilized setting. This activity took place over a very wide sector, extending east and north--eastwards from central Mongolia to the Pacific Ocean for some 2500 - 3000 km, thereby consti" . "522897" . "2005-12-14+01:00"^^ . "Alberti, C." . "Granitoidn\u00ED horniny St\u0159edomongolsk\u00E9ho vyv\u0159elinov\u00E9ho p\u00E1su"@cs . "80-7157-920-3" . "4"^^ . . "Granitoidn\u00ED horniny St\u0159edomongolsk\u00E9ho vyv\u0159elinov\u00E9ho p\u00E1su"@cs . . "Granitoids of the Central Mongolian Igneous Belt"@en . "[E5100B6C314E]" . . . "Majigsuren, Yordon" . . "Brno" . "P(GD526/03/H036)" .