Gold-bearing hydrothermal breccias of rhyodacitic composition, related to Paleozoic granitic porphyries intruded into Devonian/Carboniferous calcareous sediments and underlying rocks of the Precambrian basement.
Not to be confused with the Longtoushan deposit in the Dachang tin ore field.
Ref.:
- National Geoscience Database of Iran (www.ngdir.ir/GeoportalInfo/SubjectInfoDetail.asp?PID=331&index=25)
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Map Reference: 23°12'N , 109°27'E
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