CHADIMA, Martin, František HROUDA a Rostislav MELICHAR. Magnetic fabric study of the SE Rhenohercynian Zone (Bohemian Massif): Implications for dynamics of the Paleozoic accretionary wedge. Tectonophysics. Amsterdam: Elsevier, 2006, roč. 418, 1-2, s. 93-109, 13 s. ISSN 0040-1951. |
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@article{696312, author = {Chadima, Martin and Hrouda, František and Melichar, Rostislav}, article_location = {Amsterdam}, article_number = {1-2}, keywords = {AMS; Magnetic fabric; Accretionary wedge; Rhenohercynian Zone}, language = {eng}, issn = {0040-1951}, journal = {Tectonophysics}, title = {Magnetic fabric study of the SE Rhenohercynian Zone (Bohemian Massif): Implications for dynamics of the Paleozoic accretionary wedge}, volume = {418}, year = {2006} }
TY - JOUR ID - 696312 AU - Chadima, Martin - Hrouda, František - Melichar, Rostislav PY - 2006 TI - Magnetic fabric study of the SE Rhenohercynian Zone (Bohemian Massif): Implications for dynamics of the Paleozoic accretionary wedge JF - Tectonophysics VL - 418 IS - 1-2 SP - 93-109 EP - 93-109 PB - Elsevier SN - 00401951 KW - AMS KW - Magnetic fabric KW - Accretionary wedge KW - Rhenohercynian Zone N2 - The progressive deformation recorded in the magnetic fabric of sedimentary rocks was studied in the SE Rhenohercynian Zone (RHZ), eastern margin of the Bohemian Massif, Czech Republic. Almost 800 oriented samples of the Lower Carboniferous mudstones and graywackes were collected from the SSE part of the Czech RHZ, so-called the Drahany Upland. The anisotropy of magnetic susceptibility (AMS) is predominantly controlled by the preferred orientation of paramagnetic phyllosilicates, mainly iron-bearing chlorites. A regional distribution of the magnetic fabric within the Drahany Upland revealed an increasing deformation from the SSE to the NNW. In the SE, the magnetic fabric is bedding-parallel with magnetic lineation scattered in the bedding plane or trending N–S to NNE–SSW. Further to the NW, the magnetic foliation rotates from the bedding-parallel orientation to the orientation parallel to the evolving cleavage. ER -
CHADIMA, Martin, František HROUDA a Rostislav MELICHAR. Magnetic fabric study of the SE Rhenohercynian Zone (Bohemian Massif): Implications for dynamics of the Paleozoic accretionary wedge. \textit{Tectonophysics}. Amsterdam: Elsevier, 2006, roč.~418, 1-2, s.~93-109, 13 s. ISSN~0040-1951.
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