"Verner, Kry\u0161tof" . "17"^^ . "[316F6791AF9D]" . . . . "International Journal of Earth Sciences" . . "Plech\u00FD pluton jako sou\u010D\u00E1st z\u00E1padn\u00ED v\u011Btve Centr\u00E1ln\u00EDho moldanubick\u00E9ho batolitu je klasick\u00FDm reprezentantem pozdn\u011B-varisk\u00E9ho magmatismu v moldanubiku. Jeho st\u00E1\u0159\u00ED je nep\u0159\u00EDmo odhadov\u00E1no na ~320Ma. Jedn\u00E1 se o intruzi m\u00EDrn\u011B prota\u017Een\u00E9 geometrie (24x16km), kter\u00E1 je v ji\u017En\u00EDch parti\u00EDch ost\u0159e ohrani\u010Dena strukturou SSZ-JJV prob\u00EDhaj\u00EDc\u00ED Pf\u00E1hlsk\u00E9 st\u0159i\u017En\u00E9 z\u00F3ny. Plech\u00FD pluton je slo\u017Een ze t\u0159\u00ED variet granitov\u00E9ho magmatu S \u2013 typu:(i) st\u0159edn\u011Bzrnn\u00FD bt-mu granit s gran\u00E1tem (okrajov\u00FD granit), (ii) hrubozrnn\u00FD, slab\u011B porfyrick\u00FD mu-bt granit (granit Plech\u00FD a Haidm\u00FChler granit v N\u011Bmecku), a (iii) st\u0159edn\u011Bzrnn\u00FD, v\u00FDrazn\u011B profyrick\u00FD mu-bi granit (granit t\u0159\u00EDstoli\u010Dn\u00EDk). Variace v celkov\u00E9m chemismu hornin (zejm\u00E9na Zr, Th a REE) a obsahu miner\u00E1l\u016F (zejm\u00E9na monazitu, zirkonu a gran\u00E1tu) v r\u00E1mci d\u00EDl\u010D\u00EDch variet ukazuj\u00ED na jejich m\u00EDru diferenciace a tedy sukces\u00EDvn\u00ED st\u00E1\u0159\u00ED v \u0159ad\u011B (I-II-III). Plech\u00FD pluton d\u00E1le vykazuje velmi v\u00FDraznou t\u00EDhovou anom\u00E1lii, kter\u00E1 indikuje strm\u00E9 kontakty intruze a minim\u00E1ln\u00ED hloubkov\u00FD dosah v rozmez\u00ED 5,5-8,5km."@cs . "Pertoldov\u00E1, Jaroslava" . "Magmatic history and geophysical signature of a post-collisional intrusive center emplaced nearby a crustal-scale shear zone: the Plech\u00FD granite pluton (Moldanubian batholith, Bohemian Massif)" . . "DE - Spolkov\u00E1 republika N\u011Bmecko" . . "\u017D\u00E1k, Ji\u0159\u00ED" . . . . . "Magmatick\u00FD v\u00FDvoj a geofyzik\u00E1ln\u00ED z\u00E1znam varisk\u00E9 post-kolizn\u00ED intruze, vm\u00EDst\u011Bn\u00E9 v asociaci se st\u0159i\u017Enou z\u00F3nou korov\u00E9ho m\u011B\u0159\u00EDtka: Plech\u00FD pluton, \u010Cesk\u00FD mas\u00EDv."@cs . "Magmatick\u00FD v\u00FDvoj a geofyzik\u00E1ln\u00ED z\u00E1znam varisk\u00E9 post-kolizn\u00ED intruze, vm\u00EDst\u011Bn\u00E9 v asociaci se st\u0159i\u017Enou z\u00F3nou korov\u00E9ho m\u011B\u0159\u00EDtka: Plech\u00FD pluton, \u010Cesk\u00FD mas\u00EDv."@cs . "neuveden" . "The Plech\u00FD pluton, south-western Bohemian Massif, represents a late-Variscan, complexly zoned intrusive center emplaced near the crustal-scale Pfahl shear zone; the pluton thus provides an opportunity to examine the interplay among successive emplacement of large magma batches, magmatic fabric acquisition, and the late-Variscan stress field associated with strike-slip shearing. The magmatic history of the pluton started with the emplacement of the the porphyritic Plech\u00FD and Haidm\u00FChler granites. Based on gravity and structural data we interpret that the Plech\u00FD and Haidm\u00FChler granites were emplaced as a deeply rooted, ~NE\u2013SW elongated body; its gross shape and internal fabric (steep ~NE\u2013SW magmatic foliation) may have been controlled by the late-Variscan stress field."@en . "Magmatic history and geophysical signature of a post-collisional intrusive center emplaced nearby a crustal-scale shear zone: the Plech\u00FD granite pluton (Moldanubian batholith, Bohemian Massif)"@en . "RIV/00025798:_____/08:00000055!RIV08-MZP-00025798" . "Z(MZP0002579801)" . . "5"^^ . "377387" . . "Magmatic history and geophysical signature of a post-collisional intrusive center emplaced nearby a crustal-scale shear zone: the Plech\u00FD granite pluton (Moldanubian batholith, Bohemian Massif)"@en . . "T\u00FDcov\u00E1, Patricie" . "The Plech\u00FD pluton, south-western Bohemian Massif, represents a late-Variscan, complexly zoned intrusive center emplaced near the crustal-scale Pfahl shear zone; the pluton thus provides an opportunity to examine the interplay among successive emplacement of large magma batches, magmatic fabric acquisition, and the late-Variscan stress field associated with strike-slip shearing. The magmatic history of the pluton started with the emplacement of the the porphyritic Plech\u00FD and Haidm\u00FChler granites. Based on gravity and structural data we interpret that the Plech\u00FD and Haidm\u00FChler granites were emplaced as a deeply rooted, ~NE\u2013SW elongated body; its gross shape and internal fabric (steep ~NE\u2013SW magmatic foliation) may have been controlled by the late-Variscan stress field." . "pluton, emplacement, granite, AMS"@en . . "7"^^ . "Sedl\u00E1k, Ji\u0159\u00ED" . "Truba\u010D, Jakub" . . . "\u0160r\u00E1mek, Josef" . "Magmatic history and geophysical signature of a post-collisional intrusive center emplaced nearby a crustal-scale shear zone: the Plech\u00FD granite pluton (Moldanubian batholith, Bohemian Massif)" . "RIV/00025798:_____/08:00000055" . . . . "neuveden" . "1437-3254" . .