驼路沟钴、金矿位于东昆仑褶皱系昆南断褶带内，产于晚古生代二叠系下统石英片岩中。
Tuoluogou cobalt and gold deposit is in the south of the east Kunlun drape. It formed in quartz schist in the forepant Permian of late vecent life.
苏南的上古生代紧密褶皱、火山与岩浆活动以及二个地震活动带的存在，均与莫氏面的起伏有关。
Perhaps there are some tension fractures in it. 4. The complex folds in the upper palaeozoic, the volcano and the seismic zones may be related to the undulation of Moho discontinuity.
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