///The iron-polymetallic deposit in West Nalinggele River of Qinghai belongs to the Qimantage metallogenic belt in the western section of east Kunlun Mountain, and with favorable ore-forming condition. Due to the Gobi desert landscape and thick cover, usually 150~280 m in this region, there is no rocks and mineralization exposed. Through the high-precision measurement of magnetic and magnetic anomaly drilling authentication, the good iron-polymetallic ore bodies are found in the deep. The preliminary understanding of the geological features indicate that the iron-polymetallic deposit belongs to the skarn-type deposits, and this also means that the magnetic work in the region has achieved good results.
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