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- W2282884027 abstract "The work was focused on the Upper Proterozoic metasedimentaryrocks, studies of their anisotropy of magnetic susceptibility(AMS). Research was held in Kralupy-Zbraslav and Stěchoviceformations that are situated in Barrandian, Czech Republic.There is a 15–20 km wide and about 60 km long stripe amongPrague, Dobřis, Přibram, Rožmital pod Třemsinem and Nový Knin.About 220 oriented samples were collected by manual drillingmachine from outcrops or in laboratory from oriented blocks.AMS of drilled cores was measured in AGICO laboratories Brno onMFK1 instrument. In studied rocks were founded two types of AMSfabrics (see Fig. 1). Types are caused by different litology:fine-grained sediments are associated with oblate fabric withdominated magnetic foliation (bedding), however thecoarse-grained ones generate prolate fabric indicating strain.Two orientations of AMS fabrics, found on studied area, arepresumably called by different deformations. The most commondeformation is varisian, AMS axis are oriented NW-SE. Thisdeformation was caused by massive intrusions on NE of region.The second AMS fabric of unknown origin is oriented NE-SW.During our studies was found one site (28) with inverse fabric.This may be caused by ankerite or siderite and need furtherinvestigation." @default.
- W2282884027 created "2016-06-24" @default.
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- W2282884027 date "2015-01-01" @default.
- W2282884027 modified "2023-09-26" @default.
- W2282884027 title "AMS fabrics in the Upper Proterozoic metasediments ofBarrandian" @default.
- W2282884027 hasPublicationYear "2015" @default.
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