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祁漫塔格位于东昆仑造山带西段,该区建造组成丰富,断裂构造发育,以北西西向为主,华力西-印支造山旋回中酸性侵入岩浆活动强烈(张雪亭,2007)。区内多金属矿产找矿成果明显,但铀矿地质工作程度较低。通过近几年铀矿调查与研究,新发现一批较好铀异常点(带),本文大致总结该区铀矿化特征,
Qimantag is located in the western section of the East Kunlun orogen, and is rich in fauna and tectonic development of the fault zone, mainly in the northwestern and western directions. The acid-intrusion magmatic activity in the Waley-Indo-orogenic fold is intense (Zhang, Xueting, 2007). The discovery of polymetallic minerals in the area has obvious achievements, but the geological work of uranium deposits is relatively low. Through the investigation and study of uranium deposits in recent years, a number of new uranium anomaly spots (belts) have been newly discovered. This paper summarizes the characteristics of uranium mineralization in this area,