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Arb. Univ. Göttingen. C. & Weber, K. - This vol. Aubouin, J. - Bull. Soc. Geol. Fr. (7), 3, 629-711. Aubouin, J. - Pev. , 1, 335 pp. M. H. - 26e congr. geol. , Paris 198U, colloque C 6, Geology of Furope, 191-202. H. & Jacobshagen, V. - Z. dt. geol. Ges , 12S, 195-223. Bär, P. N. Jb. Geol. , 131/3, 263-288. A. & Montadert, L. - In: 26e congr. geol. , Paris 1980, colloque C 3,6, Geology of Continental Margins, 87-101. , Matte, P. & Rib~iro, A. - 26e congr. geol. , Paris 1980, colloque C 6, Geology of Europe, 233-246.

Pijks Geol. S. 27, (3), 81-195. , Sanchez de posada, L. & Truyols, J. - Ministere des affaires 6conomiques, Administration des Mines, Service gco10gique, Professional Paper, 1977/11, no. 148, 58 pp. Pöger, H. - Mitt. Geol. - Pa1äont. Inst. Univ. Hamburg, 50, 45-58. , Krylatov, S. & Stoppel, D. - Ceol. , P 9, 60 pp. Fuggisch, W. - Abh. hess. -A. , 62, 68 pp. P. In: European Reef flodels (F. , 30, 85-142. Burmann, G. (1973) Das Ordovizium der nördlichen Phyllitzone. Z. geol. , Thernenh. 1,1, 9-44.

Gießen-, Werra-, Südharz-, Selke-greywacke), it seems reasonable to assume that the early greywackes once were at least as important as the visean Flysch. This is in good agreement with radiometrie data (see eontribution by Weber and Pehr) whieh suggest tectonie thiekening and metamorphism in the area of the Mid German Crystalline Fise already in Devonian time. Famennian greywackes are also present within the (Bavarian) chert facies of the Saxothuringian zone, and greywackes at the Erbendorf I ine , the assl1med root- zone of the Saxothur ing ian nappes, have li kewi se produced Famenn ian conodonts (Adam and Peuter, 1981).

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Arakcheev, Grand Vizier of the Russian Empire by Michael Jenkins


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