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- W2737041883 abstract "Sedimentary rocks in Prague Synform were significantly affectedby deformation during variscan orogeny. The Silurian andDevonian rocks were intensely folded and thrusted (Melichar,2003). Unfortunately, deformation of the Ordovician rocks isnot visible. Due to observations of internal fabrics of rocks,anisotropy of magnetic susceptibility (AMS) study wasextensively used. Different types of AMS fabrics were found inthe investigated area. This study is focused on strain fabrics.Such fabrics are associated with different deformation episodesthat affected the area. Essentially, there are two groups ofstrain fabrics related to different deformation scenarios inPrague Synform. These groups differ in the orientation ofmagnetic lineation in paleocoordinates (Figure). From thatpoint of view, the AMS fabrics from the neighbour of Skřipelvillage are very important for understanding the complicatedsituation in Ordovician rocks. These results points out thateach group of strain fabrics was originated during differentdeformation." @default.
- W2737041883 created "2017-07-31" @default.
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- W2737041883 date "2015-11-05" @default.
- W2737041883 modified "2023-09-27" @default.
- W2737041883 title "Deformation of Ordovician sedimentary rocks, Prague Synform,Barrandian, Czech Republic" @default.
- W2737041883 hasPublicationYear "2015" @default.
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