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Subduction-driven shortening and differential exhumation in a Cadomian accretionary wedge: The Teplá-Barrandian unit, Bohemian Massif
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SYSNO ASEP 0334641 Document Type J - Journal Article R&D Document Type Journal Article Subsidiary J Článek ve WOS Title Subduction-driven shortening and differential exhumation in a Cadomian accretionary wedge: The Teplá-Barrandian unit, Bohemian Massif Author(s) Hajná, J. (CZ)
Žák, J. (CZ)
Kachlík, V. (CZ)
Chadima, Martin (GLU-S) RID, SAISource Title Precambrian Research. - : Elsevier - ISSN 0301-9268
Roč. 176, 1/4 (2010), s. 27-45Number of pages 19 s. Publication form WWW - WWW Language eng - English Country NL - Netherlands Keywords accretionary wedge ; anisotropy of magnetic susceptibility (AMS) ; Teplá-Barrandian unit ; Bohemian Massif ; Cadomian orogeny ; Variscan orogeny Subject RIV DE - Earth Magnetism, Geodesy, Geography CEZ AV0Z30130516 - GLU-S (2005-2011) UT WOS 000273933100003 EID SCOPUS 71949090310 DOI 10.1016/j.precamres.2009.10.009 Annotation Magnetic mineralogy of the Precambriam sediments in the Teplá–Barrandian unit was investigated for the purpose of tectonic interpretation of magnetic anisotropy. In addition to phyllosilicates, pyrrhotite and siderite was found as the carriers of magnetic fabric. Pyrrhotite and siderite-bearing samples cannot be interpreted together with phyllosilicate-bearing samples. Workplace Institute of Geology Contact Jana Popelková, popelkova@gli.cas.cz, Sabina Janíčková, Tel.: 233 087 272 Year of Publishing 2010
Number of the records: 1