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The Tianshuihai lead–zinc deposit, located in the Karakorum Mountains, Xinjiang Province, NW China, was discovered in 2011. The ore bodies occur within the clastic rocks in the lower part of the Cretaceous Tielongtan Group. The main ore body of the mineral deposit is 450m in length, 5.24–47.5m in thickness and 201m in depth. It strikes NE and dips SE at about 50°, which is consistent with the occurrence...
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