Detailed Information on Publication Record
2006
Magnetic fabric study of the SE Rhenohercynian Zone (Bohemian Massif): Implications for dynamics of the Paleozoic accretionary wedge
CHADIMA, Martin, František HROUDA and Rostislav MELICHARBasic information
Original name
Magnetic fabric study of the SE Rhenohercynian Zone (Bohemian Massif): Implications for dynamics of the Paleozoic accretionary wedge
Name in Czech
Magnetická stavba severovýchdu rhenohercynské zóny: implikace pro dynamiku paleozoického akrečního klínu
Authors
CHADIMA, Martin (203 Czech Republic), František HROUDA (203 Czech Republic) and Rostislav MELICHAR (203 Czech Republic, guarantor)
Edition
Tectonophysics, Amsterdam, Elsevier, 2006, 0040-1951
Other information
Language
English
Type of outcome
Článek v odborném periodiku
Field of Study
10500 1.5. Earth and related environmental sciences
Country of publisher
Netherlands
Confidentiality degree
není předmětem státního či obchodního tajemství
Impact factor
Impact factor: 1.675
RIV identification code
RIV/00216224:14310/06:00017229
Organization unit
Faculty of Science
UT WoS
000237459600008
Keywords in English
AMS; Magnetic fabric; Accretionary wedge; Rhenohercynian Zone
Tags
Reviewed
Změněno: 29/3/2010 12:51, doc. RNDr. Rostislav Melichar, Dr.
V originále
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.
In Czech
Bzla studována magnetická stavba severovýchodu rhenohercynské zóny a její význam pro dynamiku paleozoického akrečního klínu na Moravě.
Links
| MSM0021622412, plan (intention) |
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