Normal> Yingebulake iron deposit lies in the edge of ancient continent. Its mother rocks are the metamorphic oceanic volcanic sedimental rocks of the under segment of Zuoarbulake Formation, Jixian System, which are magnetic silicalite, siliceous slate, and magnetic phyllite. There is a typical construction of BIF for these rocks. Iron bodies are controlled by Baijianshan synclinorium. The genetic classification of this deposit is oceanic volcanic-sedimental metamorphic type which just likes the Algema type iron deposit of sedimental-metamorphic in foreign countries. There is a good potential of iron mineral exploration of this deposit.