By Peter Giese, J. Behrmann (auth.), P. Giese, J. Behrmann (eds.)
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Extra info for Active Continental Margins — Present and Past
5 b1). (3) The upper stratigraphic unit (Fig. 5b c), up to 300 m thick, consists of thin interbedded muds tones with sandstone occurrences, deposited in the area between the channels. The evolution of the Krania basin is strongly affected by two west-dipping upthrusts. The 'Krania Thrust' to the west formed during the Late Eocene (progressive subsidence including the deposition of interchannellobe and debris flow sediments adjacent to the thrust front). Later, during the latest Eocene, the Apulian Thrust to the east back-tilted the already deposited sediments in the Krania basin.
G. Platt, 1986; Royden and Burchfiel, 1987; Dewey, 1988). The present study provides evidence for such extension within the Variascan Regional geology To the west of the WBS, the Moldanubian rocks (Fig. 1) consist mainly of cordierite - sillimanite gneisses which belong to the Monotonous Series (Vejnar, 1965). , 1988). However, at least part of the paragneisses may have formed form Early Palaeozoic sediments. , 1989). At many places the cordierite-sillimanite gneisses were intruded by late to post-tectonic S-type granites.
Kontopoulos Intraeontinental wedging and post-orogenie eollapse in the Mesohellenie Trough Received: 1 lune 1993/ Accepted: 21 March 1994 Abstract The Mesohellenie Trough is a 130 km long and about 30 km wide subsiding area whieh eontains a thiek sequenee of well exposed Late Cenozoie post-orogenie sediments. This intermontane basin, loeated at the eontaet between the Apulian and Pelagonian eollided margins, provides a good example of the eharaeteristies needed to study the ehronology oflate orogenie intraeontinental structures.
Active Continental Margins — Present and Past by Peter Giese, J. Behrmann (auth.), P. Giese, J. Behrmann (eds.)