西藏措勤盆地地质特征及铀成矿远景评价  

The Geologic Feature of Tibet Coqen Basin and Uranium Metallogenic Prospecting Evaluation

作　　者：王进进[1] 陈玉梁 陈载林[3] Wang Jinjin;Chen Yuliang;Chen Zailin(Faculty of Land Resource Engineering,Kunming University of Science and Technology,Kunming 650093,China;Research Institute No. 280,CNNC,Guanghan 618300,Sichuan Chian;Yunnan Land and Resources Vocational College,Kunming 650217,China)

机构地区：[1]昆明理工大学国土资源工程学院,昆明650093 [2]核工业280研究所,四川广汉618300 [3]云南国土资源职业学院,昆明650217

出　　处：《河南科学》2016年第7期1130-1134,共5页Henan Science

基　　金：中国地质调查局项目(1212010913025)

摘　　要：西藏措勤盆地是仅次于羌塘盆地的第二大盆地,盆地盖层构造变形强烈,构造十分复杂,褶皱、断裂特别发育.对具有代表性的地层进行物探测量,各地层均表现出了良好的铀异常特征.并对盆地铀成矿远景区进行了评价,认为该盆地具有良好的铀源、地层、岩性和构造条件.Tibet Coqen basin is the second largest basin,only second to the Qiangtang Basin in our country. With severe deformation,the cover structure of its basin is much too complicated. Besides,the drape and fault develop well. Through the geophysical prospecting of the representative stratums,each stratum shows a good feature of the uranium abnormal. Based on the evaluation in the uranium metallogenic prospecting evaluation,it is thought that the basin has good uranium source,stratums,lithology and tectonic conditions.

关 键 词：地质特征 铀矿 远景评价 措勤盆地 

分 类 号：P619.14[天文地球—矿床学]