Crystalline limestone pebbles in the Devonian clastics of the Závist Unit: possible implication for tectonometamorphic and paleogeographic development of eastern margin of the Bohemian Massif

Abstract

Redeposited clasts of devonian limestones and their thin intercalations in coarse-grained clastic of the Závist unit of Tišnov Brunnides show extremely shallow water condition of these limestones and active synsedimentary tectonic movements dur

Keywords

• Devonian
• limestones
• pebbles
• Závist Unit
• Tišnov Brunnides
• Brunovistulicum