"2" . . . . "21" . "Northeastern part of the Krkono\u0161e-Jizera Unit is built of orthogneisses with presence of elongated bodies of low- to marginally medium-grade metasedimentary rocks (phyllites to mica-schists), amphibolites and metamorphic felsic rocks of uncertain origin. Regional metamorphism and polyphase deformation in the northwestern Krkono\u0161e-Jizera Unit took place during the Variscan orogeny. This metamorphic complex was intruded by high-K calc-alkaline granitoids of the Krkono\u0161e-Jizera Pluton. Temperature and pressure conditions of regional metamorphism, which have been broadly associated with the formation of moderately NW dipping foliation and SW stretching lineation, were estimated at 530-617 \u00B0C and 6-7 kbar. Regionally metamorphosed rocks subsequently underwent younger contact metamorphism in thermal aureole of posttectonically emplaced body the Krkono\u0161e-Jizera Pluton. This subsequent metamorphic event was associated with the formation of contact mineral assemblage indicating temperature in range between 541 and 685 \u00B0C and pressure around 3 kbar."@en . "Buri\u00E1nek, David" . "[EB4DE701C036]" . . "Strukturn\u00ED a metamorfn\u00ED v\u00FDvoj severoz\u00E1padn\u00ED \u010D\u00E1sti krkono\u0161sko-jizersk\u00E9ho krystalinika (v okol\u00ED L\u00E1zn\u00ED Libverda)" . "Structural and metamorphic evolution of the northwestern Krkono\u0161e-Jizera Unit (in the surrounding L\u00E1zn\u011B Libverda)"@en . "Verner, Kry\u0161tof" . "RIV/00025798:_____/13:00000531" . "3"^^ . "Mr\u00E1zov\u00E1, \u0160t\u011Bp\u00E1nka" . "CZ - \u010Cesk\u00E1 republika" . "108463" . "V hornin\u00E1ch krkono\u0161sko-jizersk\u00E9ho krystalinika na severn\u00EDm okraji krkono\u0161sko-jizersk\u00E9ho plutonu m\u016F\u017Eeme identifikovat t\u0159i metamorfn\u00ED ud\u00E1losti spojen\u00E9 s varisk\u00FDm tektonometamorfn\u00EDm v\u00FDvojem t\u00E9to jednotky. Nejstar\u0161\u00ED vysokotlak\u00E1 metamorf\u00F3za (M1) nen\u00ED ve studovan\u00FDch horninov\u00FDch vzorc\u00EDch dob\u0159e dokumentov\u00E1na (relikty metamorfn\u00EDch foliac\u00ED S1). P\u0159\u00EDtomnost muskovitu s vy\u0161\u0161\u00EDm obsahem Na a chemick\u00E9 slo\u017Een\u00ED ve st\u0159edech porfyroblast\u016F gran\u00E1tu v\u0161ak nazna\u010Duje \u017Ee ovlivnila i studovanou oblast. Podm\u00EDnky region\u00E1ln\u00ED metamorf\u00F3zy M2 (530-617 \u00B0C a 6-7 kbar) byly vypo\u010Dteny na z\u00E1klad\u011B studia miner\u00E1ln\u00EDch asociac\u00ED fylit\u016F a pararul s miner\u00E1ln\u00ED asociac\u00ED: Qtz + Ms + Pl + Grt \u00B1 Bt \u00B1 Chl \u00B1 Ilm/Rt. Strukturami relativn\u011B nejstar\u0161\u00ED jsou intenzivn\u011B zvr\u00E1sn\u011Bn\u00E9 plochy metamorfn\u00ED foliace ozna\u010Den\u00E9 jako S1. Intenzivn\u00ED p\u0159estavba do v sou\u010Dasn\u00E9 dob\u011B st\u0159edn\u011B k SZ uklon\u011Bn\u00FDch staveb (S2) vznikala v kompresn\u00EDm re\u017Eimu, kter\u00FD byl spojen s tvorbou ploch\u00E9 p\u0159\u00EDkrovov\u00E9 stavby s kinematikou p\u0159esunu k z\u00E1padu. Mlad\u0161\u00ED miner\u00E1ln\u00ED asociace M3 (Ms + Bt + Qtz + Pl + Cdr \u00B1 And \u00B1 Kfs \u00B1 Ilm) vznikla v d\u016Fsledku kontaktn\u00EDch \u00FA\u010Dink\u016F krkono\u0161sko-jizersk\u00E9ho plutonu. Pro vzorek s gran\u00E1tem se poda\u0159ilo vypo\u010D\u00EDtat PT podm\u00EDnky kontaktn\u00ED metamorf\u00F3zy na 613 \u00B1 50 \u00B0C a 3 \u00B1 1 kbar. Teploty vypo\u010Dten\u00E9 pro ostatn\u00ED vzorky kol\u00EDsaj\u00ED v z\u00E1vislosti na intenzit\u011B kontaktn\u00ED metamorf\u00F3zy (541-685 \u00B0C). Tato metamorf\u00F3za v\u00FDrazn\u011B zm\u011Bnila chemick\u00E9 slo\u017Een\u00ED \u0159ady miner\u00E1l\u016F, kter\u00E9 v hornin\u011B koexistovaly ji\u017E b\u011Bhem region\u00E1ln\u00ED metamorf\u00F3zy. B\u011Bhem kontaktn\u00ED metamorf\u00F3zy tak\u00E9 vznikal na \u00FAkor gran\u00E1tu cordierit spolu s biotitem a objevil se tak\u00E9 andalusit. V d\u016Fsledku vm\u00EDst\u011Bn\u00ED krkono\u0161sko-jizersk\u00E9ho plutonu vznikaly v metapelitech drobn\u00E9 asymetrick\u00E9 kinkov\u00E9 vr\u00E1sy a strm\u00E9 osn\u00ED kliv\u00E1\u017Ee v-z. orientace. V \u00FAzk\u00E9 z\u00F3n\u011B pod\u00E9l intruzivn\u00EDho kontaktu plutonu nab\u00FDv\u00E1 osn\u00ED kliv\u00E1\u017E charakter superponovan\u00E9 metamorfn\u00ED foliace S3. B\u011Bhem celkov\u00E9ho chladnut\u00ED komplexu doch\u00E1z\u00ED k lokalizaci deformace a p\u0159echodu ke k\u0159ehk\u00E9mu chov\u00E1n\u00ED."@cs . . . "I" . "V hornin\u00E1ch krkono\u0161sko-jizersk\u00E9ho krystalinika na severn\u00EDm okraji krkono\u0161sko-jizersk\u00E9ho plutonu m\u016F\u017Eeme identifikovat t\u0159i metamorfn\u00ED ud\u00E1losti spojen\u00E9 s varisk\u00FDm tektonometamorfn\u00EDm v\u00FDvojem t\u00E9to jednotky. Nejstar\u0161\u00ED vysokotlak\u00E1 metamorf\u00F3za (M1) nen\u00ED ve studovan\u00FDch horninov\u00FDch vzorc\u00EDch dob\u0159e dokumentov\u00E1na (relikty metamorfn\u00EDch foliac\u00ED S1). P\u0159\u00EDtomnost muskovitu s vy\u0161\u0161\u00EDm obsahem Na a chemick\u00E9 slo\u017Een\u00ED ve st\u0159edech porfyroblast\u016F gran\u00E1tu v\u0161ak nazna\u010Duje \u017Ee ovlivnila i studovanou oblast. Podm\u00EDnky region\u00E1ln\u00ED metamorf\u00F3zy M2 (530-617 \u00B0C a 6-7 kbar) byly vypo\u010Dteny na z\u00E1klad\u011B studia miner\u00E1ln\u00EDch asociac\u00ED fylit\u016F a pararul s miner\u00E1ln\u00ED asociac\u00ED: Qtz + Ms + Pl + Grt \u00B1 Bt \u00B1 Chl \u00B1 Ilm/Rt. Strukturami relativn\u011B nejstar\u0161\u00ED jsou intenzivn\u011B zvr\u00E1sn\u011Bn\u00E9 plochy metamorfn\u00ED foliace ozna\u010Den\u00E9 jako S1. Intenzivn\u00ED p\u0159estavba do v sou\u010Dasn\u00E9 dob\u011B st\u0159edn\u011B k SZ uklon\u011Bn\u00FDch staveb (S2) vznikala v kompresn\u00EDm re\u017Eimu, kter\u00FD byl spojen s tvorbou ploch\u00E9 p\u0159\u00EDkrovov\u00E9 stavby s kinematikou p\u0159esunu k z\u00E1padu. Mlad\u0161\u00ED miner\u00E1ln\u00ED asociace M3 (Ms + Bt + Qtz + Pl + Cdr \u00B1 And \u00B1 Kfs \u00B1 Ilm) vznikla v d\u016Fsledku kontaktn\u00EDch \u00FA\u010Dink\u016F krkono\u0161sko-jizersk\u00E9ho plutonu. Pro vzorek s gran\u00E1tem se poda\u0159ilo vypo\u010D\u00EDtat PT podm\u00EDnky kontaktn\u00ED metamorf\u00F3zy na 613 \u00B1 50 \u00B0C a 3 \u00B1 1 kbar. Teploty vypo\u010Dten\u00E9 pro ostatn\u00ED vzorky kol\u00EDsaj\u00ED v z\u00E1vislosti na intenzit\u011B kontaktn\u00ED metamorf\u00F3zy (541-685 \u00B0C). Tato metamorf\u00F3za v\u00FDrazn\u011B zm\u011Bnila chemick\u00E9 slo\u017Een\u00ED \u0159ady miner\u00E1l\u016F, kter\u00E9 v hornin\u011B koexistovaly ji\u017E b\u011Bhem region\u00E1ln\u00ED metamorf\u00F3zy. B\u011Bhem kontaktn\u00ED metamorf\u00F3zy tak\u00E9 vznikal na \u00FAkor gran\u00E1tu cordierit spolu s biotitem a objevil se tak\u00E9 andalusit. V d\u016Fsledku vm\u00EDst\u011Bn\u00ED krkono\u0161sko-jizersk\u00E9ho plutonu vznikaly v metapelitech drobn\u00E9 asymetrick\u00E9 kinkov\u00E9 vr\u00E1sy a strm\u00E9 osn\u00ED kliv\u00E1\u017Ee v-z. orientace. V \u00FAzk\u00E9 z\u00F3n\u011B pod\u00E9l intruzivn\u00EDho kontaktu plutonu nab\u00FDv\u00E1 osn\u00ED kliv\u00E1\u017E charakter superponovan\u00E9 metamorfn\u00ED foliace S3. B\u011Bhem celkov\u00E9ho chladnut\u00ED komplexu doch\u00E1z\u00ED k lokalizaci deformace a p\u0159echodu ke k\u0159ehk\u00E9mu chov\u00E1n\u00ED." . "Bulletin mineralogicko-petrologick\u00E9ho odd\u011Blen\u00ED N\u00E1rodn\u00EDho muzea v Praze" . "3"^^ . . . "1211-0329" . . . . . . "12"^^ . "Strukturn\u00ED a metamorfn\u00ED v\u00FDvoj severoz\u00E1padn\u00ED \u010D\u00E1sti krkono\u0161sko-jizersk\u00E9ho krystalinika (v okol\u00ED L\u00E1zn\u00ED Libverda)"@cs . . . "Strukturn\u00ED a metamorfn\u00ED v\u00FDvoj severoz\u00E1padn\u00ED \u010D\u00E1sti krkono\u0161sko-jizersk\u00E9ho krystalinika (v okol\u00ED L\u00E1zn\u00ED Libverda)" . . "Strukturn\u00ED a metamorfn\u00ED v\u00FDvoj severoz\u00E1padn\u00ED \u010D\u00E1sti krkono\u0161sko-jizersk\u00E9ho krystalinika (v okol\u00ED L\u00E1zn\u00ED Libverda)"@cs . . "Structural and metamorphic evolution of the northwestern Krkono\u0161e-Jizera Unit (in the surrounding L\u00E1zn\u011B Libverda)"@en . . "RIV/00025798:_____/13:00000531!RIV15-MSM-00025798" . "European Variscides, Western Sudetes, metapelites, metamorphic fabric, contact aureole, P-T conditions"@en . .