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Introduction

  • W. Franke
Part of the IGCP-Project 233 book series (IGCP 233)

Abstract

The Saxothuringian Zone of Kossmat (1927) is one of the most complex parts of the Variscan Belt in central Europe. It consists of a northwestern crystalline belt, the Mid-German Crystalline High (Chap. IV), and a southeastern part dominated by relatively low-grade sedimentary and volcanic rocks. These sequences have been laid down in a Cambrian through to Devonian rift basin, which was closed in Devonian to Early Carboniferous time — we refer to this as the Saxothuringian Basin.

Keywords

Early Carboniferous Accretionary Wedge Clastic Sediment Late Ordovician Angular Unconformity 
These keywords were added by machine and not by the authors. This process is experimental and the keywords may be updated as the learning algorithm improves.

References

  1. Kossmat F (1927) Gliederung des varistischen Gebirgsbaues. Abh Sächs Geol Landesamt NF 1: 39 ppGoogle Scholar
  2. Suess F-E (1912) Vorläufige Mitteilung über die Münchberger Deckscholle. Sitzungsber Akad Wiss Wien, Math-Naturwiss Kl 121 Abt IIa(10): 253Google Scholar

Copyright information

© Springer-Verlag Berlin Heidelberg 1995

Authors and Affiliations

  • W. Franke

There are no affiliations available

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