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The Early Miocene Olistostromes and "Old Styrian Overthrusting" in the Polish Western Carphatians
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Geolines
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January 1, 2005
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Copyright informationCopyright Institute of Geology 2005. Provided by ProQuest LLC. (Hide copyright information)
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The Lower Miocene, autochthonous deposits from the basement of the Flysch Western Carpathians in Poland have been known since the late 1970's. The deposits were documented in the following deep boreholes: Bielsko 4, Sucha IG 1, Zawoja 1, Lachowice 1, 2, 3a, 7, Cieszyn IG 1, Bielowicko IG 1 and Zebrzydowice 13 (see Oszczypko and Oszczypko-Clowes 2003, Slaczka and Oszczypko 1987, and bibliography therein). The oldest known deposits of the Zawoja Fm. probably belong to the Oligocene (Egerian). In the middle part of this formation a 43 m strongly, folded flysch olistostrome (Palaeocene-Middle Eocene) was pierced.
The Sucha Formation, which was identified in the given boreholes, overlaps the ...
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