ČERNÝ, Jan a Rostislav MELICHAR. Deformation of Ordovician sedimentary rocks, Prague Synform, Barrandian, Czech Republic. In 13th Meeting of the Central European Tectonic Studies Group. 2015. ISBN 978-80-7075-880-9.
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Základní údaje
Originální název Deformation of Ordovician sedimentary rocks, Prague Synform, Barrandian, Czech Republic
Autoři ČERNÝ, Jan (203 Česká republika, garant, domácí) a Rostislav MELICHAR (203 Česká republika, domácí).
Vydání 13th Meeting of the Central European Tectonic Studies Group. 2015.
Další údaje
Originální jazyk angličtina
Typ výsledku Konferenční abstrakt
Obor 10500 1.5. Earth and related environmental sciences
Stát vydavatele Česká republika
Utajení není předmětem státního či obchodního tajemství
WWW Odkaz na PDF verzi sborníku
Kód RIV RIV/00216224:14310/15:00082846
Organizační jednotka Přírodovědecká fakulta
ISBN 978-80-7075-880-9
Klíčová slova anglicky Anisotropy of magnetic susceptibility; AMS; Ordovician; Prague synform; Tectonics; Structural geology; Sedimentary rock
Změnil Změnil: Mgr. Jan Černý, Ph.D., učo 176111. Změněno: 11. 5. 2015 12:03.
Anotace
Sedimentary rocks in Prague Synform were significantly affected by deformation during variscan orogeny. The Silurian and Devonian rocks were intensely folded and thrusted (Melichar, 2003). Unfortunately, deformation of the Ordovician rocks is not visible. Due to observations of internal fabrics of rocks, anisotropy of magnetic susceptibility (AMS) study was extensively used. Different types of AMS fabrics were found in the investigated area. This study is focused on strain fabrics. Such fabrics are associated with different deformation episodes that affected the area. Essentially, there are two groups of strain fabrics related to different deformation scenarios in Prague Synform. These groups differ in the orientation of magnetic lineation in paleocoordinates (Figure). From that point of view, the AMS fabrics from the neighbour of Skřípel village are very important for understanding the complicated situation in Ordovician rocks. These results points out that each group of strain fabrics was originated during different deformation.
VytisknoutZobrazeno: 27. 4. 2024 02:54