File:Roterkamm.jpg
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Summary
| Description |
English: "Roter Kamm" fault in Bad Schlema, Germany: The quartz-hematite mineralised Roter Kamm fault is the central element of the Gera-Jachymov fault zone hosting the largest uranium deposits of central Europe. The vertical displacement in Bad Schlema is 400m with Variscan granites on the left and phyllites on the right. The fault is the boundary between the Schneeberg Ag-Co-Ni-U and Schlema-Alberoda U deposits. Deutsch: Aufgeschlossener Ausbiss des Roten Kammes, eines hydrothermalen Quarz-Hämatitganges, der ein zentrales Element der variszisch angelegten Gera-Jáchymov-Störungszone ist, bei Bad Schlema, Erzgebirge, Sachsen. |
| Date | |
| Source | Own work |
| Author | Geomartin |
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Permission is granted to copy, distribute and/or modify this document under the terms of the GNU Free Documentation License, Version 1.2 or any later version published by the Free Software Foundation; with no Invariant Sections, no Front-Cover Texts, and no Back-Cover Texts. A copy of the license is included in the section entitled GNU Free Documentation License. |
  
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File history
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| Date/Time | Thumbnail | Dimensions | User | Comment | |
|---|---|---|---|---|---|
| current | 12:23, 1 May 2009 | | 966 × 1,482 (1.62 MB) | Daniel 1992 | Reverted to version as of 02:25, 24 April 2009 |
| 12:22, 1 May 2009 |  | 966 × 1,482 (1.63 MB) | Daniel 1992 | Version without text from German wikipedia | |
| 02:25, 24 April 2009 |  | 966 × 1,482 (1.62 MB) | Geomartin | {{Information |Description={{en|1="Roter Kamm" fault in Bad Schlema, Germany: The quartz-hematite mineralised Roter Kamm fault is the central element of the Gera-Jachymov fault zone hosting the largest uranium deposits of central Europe. The vertical disp |
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