A736 Goldschmidt Conference Abstracts 2007 Wilhemine copper mine, Spessart, Micro-Raman and Bavaria: A Kupferschiefer-related, cathodoluminescence hydrothermal mineralization characterization of shocked quartz 1 2 MARTIN OKRUSCH , JOACHIM LORENZ AND from impact craters 3 STEFAN WEYER 1 2 1 T. OKUMURA , A. GUCSIK , H. NISHIDO , 3 4 1Mineralogisches Institut, Universität Würzburg, K. NINAGAWA AND M. SAKAMOTO Am Hubland, D-97074 Würzburg, Germany 1Research Institute of Natural Sciences, Okayama University (
[email protected]) of Science, Okayama, Japan (
[email protected], 2Joachim A. Lorenz, Graslitzer Str. 5, D-63791, Karlstein am
[email protected]) Main, Germany (
[email protected]) 2Max Planck Institute for Chemistry, Department of 3Institut für Petrologie, Geochemie und Lagerstättenkunde, Geochemistry, Mainz, Germany Universität Frankfurt am Main, Senckenberganlage 28, D- (
[email protected]) 60325 Frankfurt am Main, Germany 3Department of Applied Physics, Okayama University of (
[email protected]) Science, Okayama, Japan (
[email protected]) 4Shimohisakata Elementary School, Nagano, Japan The vein-type copper mineralization in the abandoned Wilhelmine copper mine at Sommerkahl is hosted by ortho- Introduction gneisses of the Spessart Crystalline Complex. These are Evidence of shock metamorphism can be sufficiently covered by sedimentary rocks of Permo-Triassic age, proved by the existence of planar deformation features (PDFs) including the stratabound base-metal mineralization of the