Transparent to whitish barite mineralization was found in an
orogenic late phase leached fault zone. It seems that some of the barites are
pseudomorphs replaced by snow white baritocalcite. This replacement supposedly
took place at an even later phase when calcium-rich fluids migrated through the
formation. This theory is supported by the occurrence of floater quartz
crystals in a pocket where, on the one side, the quartz aggregates display the
luster of ‘bergkristall’ and are coated on t...
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