 | Staude, Sebastian, Werner, Wolfgang, Mordhorst, Teresa, Wemmer, Klaus, Jacob, Dorrit E., Markl, Gregor (2012) Multi-stage Ag–Bi–Co–Ni–U and Cu–Bi vein mineralization at Wittichen, Schwarzwald, SW Germany: geological setting, ore mineralogy, and fluid evolution. Mineralium Deposita, 47 (3) 251-276 doi:10.1007/s00126-011-0365-4 | Journal (article/letter/editorial) | | vein mineralization at Wittichen, Schwarzwald, SW Germany: geological setting, ore mineralogy, and fluid...Co–Ag–Bi–U mining area (Schwarzwald ore district, SW Germany) hosts several unconformity-related vein-type mineralizations...72074 Tübingen, Germany e-mail: markl@uni-tuebingen.de W. Werner Regierungspräsidium Freiburg, Landesamt für...und Bergbau (LGRB), Albertstr. 5, 79104 Freiburg i. Br., Germany U–Bi, Bi–Ag, Ni–As–Bi and Co–As–Bi. Important...Göttingen, Goldschmidtstr. 1-3, 37077 Göttingen, Germany Keywords Bi–Co–Ni–Ag–U vein mineralization . Schwarzwald |  | Staude, S., Mordhorst, T., Neumann, R., Prebeck, W., Markl, G. (2010) Compositional variation of the tennantite–tetrahedrite solid-solution series in the Schwarzwald ore district (SW Germany): The role of mineralization processes and fluid source. Mineralogical Magazine, 74 (2) 309-339 doi:10.1180/minmag.2010.074.2.309 | Journal (article/letter/editorial) | | solidsolution series in the Schwarzwald ore district (SW Germany): The role of mineralization processes and fluid...Tübingen, Wilhelmstrasse 56, D-72074 Tübingen, Germany [Received 30 October 2009; Accepted 28 April 2010]...locations in the Schwarzwald ore district of SW Germany. Electron microprobe analysis is used to correlate...sediments. The basement is subdivided into the Baden-BadenZone (BBZ) in the North (belonging to the Saxothuringian)...1980). From the Middle Triassic to Jurassic, SW Germany was part of a shelf platform with distinct time |  | Wagner, Thomas, Okrusch, Martin, Weyer, Stefan, Lorenz, Joachim, Lahaye, Yann, Taubald, Heiner, Schmitt, Ralf T. (2010) The role of the Kupferschiefer in the formation of hydrothermal base metal mineralization in the Spessart ore district, Germany: insight from detailed sulfur isotope studies. Mineralium Deposita, 45 (3) 217-239 doi:10.1007/s00126-009-0270-2 | Journal (article/letter/editorial) | | metal mineralization in the Spessart ore district, Germany: insight from detailed sulfur isotope studies Thomas...Springer-Verlag 2009 Abstract The Spessart district (SW Germany), located at the southwestern margin of the Permian...Universität Würzburg, Am Hubland, 97074 Würzburg, Germany S. Weyer : Y. Lahaye Institut für Petrologie, Geochemie...Senckenberganlage 28, 60325 Frankfurt am Main, Germany H. Taubald Institut für Geowissenschaften, Universität...Universität Tübingen, Wilhelmstr. 56, 72074 Tübingen, Germany R. T. Schmitt Museum für Naturkunde, Leibniz-Institut |  | | Journal (article/letter/editorial) | | vein mineralization, Bieber deposit, Spessart, Germany T. WAGNER1,2,* AND J. LORENZ3 1 Mineralogisches...Universität Würzburg, Am Hubland, D-97074 Würzburg, Germany Department of Earth and Planetary Sciences, McGill...Graslitzer Str. 5, D-63791 Karlstein am Main, Germany 2 ABSTR ACT Post-Variscan vein-type Co-Ni-Bi...ores of the Bieber deposit, Spessart mountains, Germany, which are related to the Permian Kupferschiefer...Okrusch (1965). 386 CO -NI-BI VEIN MINERALIZATION,GERMANY lowermost part of the Zechstein dolomite is composed |  | | Journal (article/letter/editorial) | | "pinge." On accountof its former copperoutput, the mine has receivedthe name "Sadisdorf CopperMine." In...but characterizedby the presenceof bismuthand bismuthinite. The hanging-wallcountryrock is a very much...in molybdenite and wolframite. The outputof this mine in •9o7 was nearly 3-4 t. wolframite and •.3 t....given rise to the name "Altenberg Zwitterstock." The mine exposuresshow that this impregnation has been confined...chamberswere formed,and one of the interestingsightsin the mine to-dayare severalof these old domeswhich are still |  | | Journal (article/letter/editorial) | | originated there by supergene alteration of bismuthinite or other primary Bi sulphides. Key words: bismutite...popisovány krásné hematitové lebníky (např. z dolu Hilfe Gottes). Železná ruda se zde dobývala od počátku 16...m. Mocnost žíly kolísala - v úrovni štoly Segen Gottes 4 - 6 m, ve štole Concordia 6 m a na dole Terezie...manganu. V roce 1917 se těžba přenesla do štoly Segen Gottes, kde se měsíčně dobývalo zhruba 50 tun bohaté rudy |  | | Book (volume) | | Deposits The Iron Ore Deposits of the Arendal Region in Norway of Krivoi-Rog, in Southern Russia Iron...Deposits of Pitkaranta in Finland 4. Kallmora Silver Mine at Norberg, in Sweden 5. The Deposit of Schneeberg...Type 4. The Gold Deposits of Zell, in the Ziller Valley, Austria 1. 2. 471 471 472 474 475 Gold-bearing...Iron Ore Deposits in the Zechstein Dolomite of the Region of Schmalkalden 6. The Iron Ore Deposits of Amberg... The Zinc and Lead Deposits of the Mississippi Valley 5. The Zinc Deposits of Iserlohn, Prussia 6. The |  | | Book | | Congress Catalog Card No. 66-17809 Printed in Germany 08 011635 3 PREFACE TO THE T H I R D (GERMAN)...N , Troy, New York, USA G. FRIEDRICH, Aachen, Germany H . FROHBERG, Toronto, Canada R. L A GANZA, North...Pullman, Washington R. A. ZIMMERMANN, Heidelberg, Germany 2 Bamdohr, Theorie Minerals XVÜ ABBREVIATIONS...places of extreme differentiation (e.g., at the Frood Mine and at Insizwa) bismuth and tellurium minerals are...H E ORE MINERALS FIG. 4 80 X Mouat Mine, Stillwater Valley, Montana RAMDOHR From a border zone, |  | | Book | | Franz J. Dahlkamp OlbergstraBe 10 D-5307 Wachtberg Germany ISBN 978-3-642-08095-1 Library of Congress Cataloging...Basins, USA), Hruby J. (CSFR), Kolb S. (Bavaria, W-Germany), Krol W. (Eastern Europe), Matos Dias J.H. (Portugal)...Canada), Ruzicka V. (CSFR), Saucier A.E. (Grants Region, N.M., USA), Smith RB. (South Texas, USA), Tan...Uranium Deposits (Type 1, Chap. 4): Athabasca Basin Region, Canada..........................................Deposits in Albitized Metasediments: Uranium City Region, Canada....................................... |
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