By Peter Giese, J. Behrmann (auth.), P. Giese, J. Behrmann (eds.)
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Additional info for Active Continental Margins — Present and Past
9), a dense set of east - west trending strike-slip faults is developed. Many of these faults displaya strong reverse component of movements and are associated with thick cataclastites and small-scale flower structures. However, together with oblique reverse faults, the occurrence of some minor faults with anormal component of movement can be interpreted as en echelon structures. At the northern termination of the trough, near leropygi village, a north-west trending set of strike-slip faults (Figs 8 1 and 10a) separates the trough infill from the Pelagonian basement.
After geological map of eS FR, 1: 500 000, western part; dashed rectangle shows outline of Fig. 2. BaPf = Bavarian Quartz Lode; CBS = Central Bohemian Shear Zone; FL = fauIt system of Franconian Line; WBS = West Bohemian Shear Zone ; ZEV = Zone of Erbendorf - Vohenstrauss; and ZTM = Zone of Tirschenreuth - Mähring internides. It focuses on the kinematics and the metamorphic evolution of the West Bohemian Shear Zone (WBS) which, as a large-scale late Variscan normal fault, separates the Moldanubian terrane from the Tepla- Barrandian terrane at the western border of the Bohemian Massif (Fig.
1) The lower stratigaphic unit crops out at the surface in the eastern part ofthe basin (Fig. 5b a). It consists ofthin to medium interbedded, up to 200 m thick, sandstone and mudstone interchannel deposits (Tab Bouma intervals, after Bouma 1962). (2) The middle stratigraphic unit consists of thin to thick interbedded, up to 300 m thick (Fig. 5 b b2) mudstone - sandstone sediments (ratio changes upwards from 1: 1 to 1: 9) (Tabc/Tbc or Tbce, Bouma intervals) deposited as lobe deposits. This unit passes laterally, adjacent to the Krania Thrust front, to debris flow conglomerates up to 40 m thick (Fig.
Active Continental Margins — Present and Past by Peter Giese, J. Behrmann (auth.), P. Giese, J. Behrmann (eds.)