The Upper Oligocene-Lower Miocene Krosno lithofacies in the Carpathian Flysch Belt (Czech republic): sedimentology, provenance and magnetic fabrics

Abstract

The investigation of translucent heavy minerals produced evidence of different spectra between the Krosno lithofacies and underlying strata of individual tectonofacial units

Keywords

• Upper Oligocene-Lower Miocene
• Carpathians
• Flysch Belt
• Krosno lithofacies
• tectonics
• paleogeography
• sedimentology
• heavy minerals
• magnetic anisotropy