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Part of the book series: IGCP-Project 233 ((IGCP 233))

Abstract

The Moldanubian Zone of the Bohemian Massif represents a major crystalline segment within the eastern part of the mid-Paleozoic Variscan fold-belt. It adjoins with the Saxo-Thuringicum to the NW, with the Bohemicum to the N, and with the Moravo-Silesian Zone to the E. The continuation of the Moldanubian Zone to the S and SW is covered by post-Variscan platform sediments.

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Fiala, J., Fuchs, G., Wendt, J.I. (1995). Stratigraphy. In: Dallmeyer, R.D., Franke, W., Weber, K. (eds) Pre-Permian Geology of Central and Eastern Europe. IGCP-Project 233. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-77518-5_42

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  • DOI: https://doi.org/10.1007/978-3-642-77518-5_42

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