Die Tektonik des Bayerischen Pfahls |
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| Authors: | Dr Richard Hofmann Diplom-Geologe |
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| Institution: | (1) Obb., Münchener Str. 2, Freising;(2) Gewerkschaft Brunhilde, Buschhof, Post Uetze, Hann. |
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| Abstract: | The dyke-quartz-masses of the Bavarian “Pfahl” are embedded in schists striking NW-SE. The Pfahl consists of numerous individual veins arranged en echelon and represents a system of feather joints which originated during a weak phase of compression normal to a NW-SE-striking axis. The age of these movements is possibly Sudetic. Post-Cretaceous movements along the north edge of the Bodenwöhr-Basin had little or no effect upon the Pfahl. There is no post-Cretaceous quartz-precipitation. |
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