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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.
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Author Geomartin

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Date/TimeThumbnailDimensionsUserComment
current12:23, 1 May 2009Thumbnail for version as of 12:23, 1 May 2009966 × 1,482 (1.62 MB)Daniel 1992Reverted to version as of 02:25, 24 April 2009
12:22, 1 May 2009Thumbnail for version as of 12:22, 1 May 2009966 × 1,482 (1.63 MB)Daniel 1992Version without text from German wikipedia
02:25, 24 April 2009Thumbnail for version as of 02:25, 24 April 2009966 × 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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