Pre-Permian Geology of Central and Eastern Europe by R.D. Dallmeyer, W. Franke, K. Weber

By R.D. Dallmeyer, W. Franke, K. Weber

In August 1990, undertaking 233 of the overseas Geological Correlation application hosted a global convention in G6ttingen/Giessen, Germany. Discussions have been curious about the Tectonothermal and Stratigraphic Evolution of the important ecu Orogens. The assembly marked the 1st chance for thoroughly open medical trade following the new political reformations in imperative Europe. This interesting new surroundings of foreign cooperation led to presentation of a wealth of data which used to be new to scientists from each side of former political limitations. It was once obvious specified chance used to be to be had to arrange a scientific evaluate in a quantity facing the geology of important Europe. the current e-book represents an outgrowth of this convention, yet isn't really only a compilation of the papers awarded in G6ttingen/Giessen. as a substitute, it represents a coordinated quantity designed to provide a balanced, entire view of our current figuring out of the tectonothermal and stratigraphic evolution of the primary eu orogens. We gratefully recognize the aid of the nationwide investment enterprises, who've financed a lot of the study paintings summarized during this ebook, and of the Interna­ tional Geological Correlation Programme (IGCP, venture no. 233) which supplied and helped to finance the organisational framework. we're indebted to Springer-Verlag for thorough copy-editing and construction of this booklet, and we truly get pleasure from the efforts of the entire reviewers whose com­ ments have significantly helped to enhance the standard of this quantity. We additionally thank a few of the individuals for his or her diligence and perseverance in manuscript practise.

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P'''' ~:.. ~V. S· ... -.. / ~/C)/ ..... ~O<' ~~4,~,,--, / I "-'~ .. . ",,,,~" ~~. ' ...... ~' ,,#",. ,"'" '... "c .... ::> . 'i,';..... :? ,~/" _ . . Rhenish Massif (E Part) and Related Areas ment (DEKORP Research Group, Franke et al. 1990). 2 Initial Rifting and Neritic Clastic Sedimentation Notwithstanding the age and composition of the underlying basement, it can be stated that the Devonian record is controlled by a major phase of crustal extension.

EIJ 0.. : : : ~, ~ E o o .. ne 'ii5::i{~:;;_-::~ 8'" . . . ~- - .... '" 2>0 .. . . . + . . - ... • ••• _... "" "" ,. N ; _ R,... ;{tw~~~~~~~L@ 63----·- ' -- --_ = __ ______ - ........ -..... -_ .... ,. , ---- - ___63_ r- ~ 201-- 54 6g a N 16 Main Features of Geophysical Structures in Central Europe of the Alps and the Baltic Sea near Kiel was the target of a detailed seismic refraction survey in 1986 (EUGEMI Working Group 1990; Aichroth and Prodehl 1990; Aichroth et al. 1992; Prodehl and Aichroth 1992).

L . ::. " . '. , SSE Fig. 8. Line drawing of the DEKORp·2 seismic reflection line, which runs from NNW to SSE between the Northern German Basin and the Danube in southern Germany (Meissner and Bortfeld 1990), The position of this line is shown in Fig, 1. The upper section covers the line between the Northern German Basin and the southern margin of the Rhenish Massif, the lower section is situated in southern Germany and passes the Saxothuringian and the Moldanubian zone TWT • 4 o .

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