"5"^^ . . "RIV/00025798:_____/14:00000212!RIV15-MSM-00025798" . "Magnetick\u00E9 stavby (AMS) granitoidn\u00EDch a gabroidn\u00EDch hornin nasavrck\u00E9ho plutonick\u00E9ho komplexu v \u017Delezn\u00FDch hor\u00E1ch"@cs . "The Nasavrky Plutonic complex crops out in the central and south-eastern parts of the \u017Delezn\u00E9 Mts. between two major lithological units: the Bohemicum or Barrandian s.l. at the north, and the Moldanubian at the south. The igneous complex appears as a polyphase intrusion of Variscan calc-alkaline granitoid and gabbroic magmas. The igneous complex is divided into three E-W trending lithological belts: southern belt of granodiorites (older and younger), central belt of gabbroic rock and northern belt of biotite granites. The fabrics of granitoides and gabbroic rocks were investigated by means of anisotropy of magnetic susceptibility (AMS). The magnetic fabrics in the older granodiorite are generally very steep up to vertical and parallel to those in their mafic microgranular enclaves (MME) and were formed during the magma emplacement. The magnetic foliation in the younger granodiorite is very variable and different from the older granodiorite and the magnetic lineation is mostly very flat. The degree of AMS is low and corresponds to the magma flow. The fabrics of gabbroic rocks of the central belt are consistent with its E-W orientation with variable dips. The orientations of magnetic foliation and lineation in biotite granite of the northern belt are variable but predominantly steep. The biotite granite shows lower degree of AMS than the gabbroic rocks."@en . . "http://www.geology.cz" . . . "0514-8057" . "Magnetick\u00E9 stavby (AMS) granitoidn\u00EDch a gabroidn\u00EDch hornin nasavrck\u00E9ho plutonick\u00E9ho komplexu v \u017Delezn\u00FDch hor\u00E1ch"@cs . "Magnetick\u00E9 stavby (AMS) granitoidn\u00EDch a gabroidn\u00EDch hornin nasavrck\u00E9ho plutonick\u00E9ho komplexu v \u017Delezn\u00FDch hor\u00E1ch" . "Nasavrck\u00FD plutonick\u00FD komplex se nach\u00E1z\u00ED v centr\u00E1ln\u00ED a jv. \u010D\u00E1sti \u017Delezn\u00FDch hor mezi dv\u011Bma litologick\u00FDmi jednotkami: bohemikem, resp. Barrandienem s.l. na severu a moldanubikem na jihu. V nasavrck\u00E9m plutonick\u00E9m komplexu, kter\u00FD je tvo\u0159en varisk\u00FDmi, v\u00E1penato-alkalick\u00FDmi granitoidn\u00EDmi a gabroidn\u00EDmi intruzemi jsou rozli\u0161eny t\u0159i v.-z. orientovan\u00E9 horninov\u00E9 p\u00E1sy, ji\u017En\u00ED granodioritov\u00FD, centr\u00E1ln\u00ED gabroidn\u00ED a severn\u00ED granitov\u00FD. Stavba granitoid\u016F i gabroid\u016F byla studov\u00E1na anizotropi\u00ED magnetick\u00E9 susceptibility (AMS). Magnetick\u00E1 stavba intruze star\u0161\u00EDho granodioritu, kter\u00E1 je p\u0159ev\u00E1\u017En\u011B strm\u00E1 a\u017E vertik\u00E1ln\u00ED, paraleln\u00ED s jeho mafick\u00FDmi mikrogranul\u00E1rn\u00EDmi enkl\u00E1vami vznikla b\u011Bhem vm\u00EDst\u011Bn\u00ED magmatu. Magnetick\u00E1 foliace mlad\u0161\u00EDho granodioritu je variabiln\u00ED a odli\u0161n\u00E1 od stavby star\u0161\u00EDho granodioritu. Magnetick\u00E1 lineace je velmi ploch\u00E1. Stupe\u0148 AMS je n\u00EDzk\u00FD a odpov\u00EDd\u00E1 magmatick\u00E9mu toku. Stavby gabroid\u016F centr\u00E1ln\u00EDho p\u00E1su jsou shodn\u00E9 s jeho v.-z. orientac\u00ED, maj\u00ED variabiln\u00ED sklony. Orientace magnetick\u00E9 foliace a lineace biotitick\u00E9ho granitu severn\u00EDho p\u00E1su jsou variabiln\u00ED, p\u0159edev\u0161\u00EDm strm\u00E9. Biotitick\u00FD granit m\u00E1 n\u00EDzk\u00FD stupe\u0148 AMS ne\u017E maj\u00ED gabroidy." . "Magnetic fabrics (AMS) of the granitoides and gabbroic rocks of the Nasavrky Plutonic Complex, \u017Delezn\u00E9 hory Mts."@en . "Hrouda, Franti\u0161ek" . . . "Chlup\u00E1\u010Dov\u00E1, Marta" . . "CZ - \u010Cesk\u00E1 republika" . "Schulmann, Karel" . . . "Magnetick\u00E9 stavby (AMS) granitoidn\u00EDch a gabroidn\u00EDch hornin nasavrck\u00E9ho plutonick\u00E9ho komplexu v \u017Delezn\u00FDch hor\u00E1ch" . "Mr\u00E1zov\u00E1, \u0160t\u011Bp\u00E1nka" . "Nasavrck\u00FD plutonick\u00FD komplex se nach\u00E1z\u00ED v centr\u00E1ln\u00ED a jv. \u010D\u00E1sti \u017Delezn\u00FDch hor mezi dv\u011Bma litologick\u00FDmi jednotkami: bohemikem, resp. Barrandienem s.l. na severu a moldanubikem na jihu. V nasavrck\u00E9m plutonick\u00E9m komplexu, kter\u00FD je tvo\u0159en varisk\u00FDmi, v\u00E1penato-alkalick\u00FDmi granitoidn\u00EDmi a gabroidn\u00EDmi intruzemi jsou rozli\u0161eny t\u0159i v.-z. orientovan\u00E9 horninov\u00E9 p\u00E1sy, ji\u017En\u00ED granodioritov\u00FD, centr\u00E1ln\u00ED gabroidn\u00ED a severn\u00ED granitov\u00FD. Stavba granitoid\u016F i gabroid\u016F byla studov\u00E1na anizotropi\u00ED magnetick\u00E9 susceptibility (AMS). Magnetick\u00E1 stavba intruze star\u0161\u00EDho granodioritu, kter\u00E1 je p\u0159ev\u00E1\u017En\u011B strm\u00E1 a\u017E vertik\u00E1ln\u00ED, paraleln\u00ED s jeho mafick\u00FDmi mikrogranul\u00E1rn\u00EDmi enkl\u00E1vami vznikla b\u011Bhem vm\u00EDst\u011Bn\u00ED magmatu. Magnetick\u00E1 foliace mlad\u0161\u00EDho granodioritu je variabiln\u00ED a odli\u0161n\u00E1 od stavby star\u0161\u00EDho granodioritu. Magnetick\u00E1 lineace je velmi ploch\u00E1. Stupe\u0148 AMS je n\u00EDzk\u00FD a odpov\u00EDd\u00E1 magmatick\u00E9mu toku. Stavby gabroid\u016F centr\u00E1ln\u00EDho p\u00E1su jsou shodn\u00E9 s jeho v.-z. orientac\u00ED, maj\u00ED variabiln\u00ED sklony. Orientace magnetick\u00E9 foliace a lineace biotitick\u00E9ho granitu severn\u00EDho p\u00E1su jsou variabiln\u00ED, p\u0159edev\u0161\u00EDm strm\u00E9. Biotitick\u00FD granit m\u00E1 n\u00EDzk\u00FD stupe\u0148 AMS ne\u017E maj\u00ED gabroidy."@cs . "26923" . "[3F5AF2AC81F2]" . "podzim" . . "I" . . . "Magnetic fabrics (AMS) of the granitoides and gabbroic rocks of the Nasavrky Plutonic Complex, \u017Delezn\u00E9 hory Mts."@en . . "2"^^ . . . "Neuveden" . "4"^^ . "Zpr\u00E1vy o geologick\u00FDch v\u00FDzkumech v roce 2013" . . "AMS, granitoides, gabbroic rock, Nasavrky Plutonic Complex, \u017Delezn\u00E9 hory Mts."@en . "RIV/00025798:_____/14:00000212" . .