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Subduction-driven shortening and differential exhumation in a Cadomian accretionary wedge: The Teplá-Barrandian unit, Bohemian Massif
- 1.0334641 - GLÚ 2010 RIV NL eng J - Journal Article
Hajná, J. - Žák, J. - Kachlík, V. - Chadima, Martin
Subduction-driven shortening and differential exhumation in a Cadomian accretionary wedge: The Teplá-Barrandian unit, Bohemian Massif.
Precambrian Research. Roč. 176, 1/4 (2010), s. 27-45. ISSN 0301-9268. E-ISSN 1872-7433
Institutional research plan: CEZ:AV0Z30130516
Keywords : accretionary wedge * anisotropy of magnetic susceptibility (AMS) * Teplá-Barrandian unit * Bohemian Massif * Cadomian orogeny * Variscan orogeny
Subject RIV: DE - Earth Magnetism, Geodesy, Geography
Impact factor: 4.116, year: 2010
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.
Permanent Link: http://hdl.handle.net/11104/0179323
Number of the records: 1