The orefield structures of the Leqingla lead-zinc deposit in Lhunzhub, Xizang

The orefield structures of the Leqingla lead-zinc deposit in Lhunzhub, Xizang are examined on the basis of 1:50 000 Geological Map and geological engineering, geophysical and geochemical prospecting. Unlike the volcanic-type kuroko deposit, the Leqingla lead-zinc deposit is believed to be associated with not volcanic activity but the emplacement of granodiorites. The mineralization is generally constrained by the EW-trending faults; the lead-zinc ores commonly appear on the footwall of the faults.