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《Journal of Nanjing University(Natural Sciences)》 1984-03
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A STUDY ON THE ISOTOPIC GEOLOGY OF No376 URANIUM DEPOSIT

Zhang Zuhuan Shen Weizhou Rao Bing  
№376 uranium deposit described in this paper is located at the endoand exo-contact zone of M rock body of Xuefeng age. Metallogenic epoch belongs to Late-Caledonian. According to Rb—Sr K—At and U—Pb isotopic dating, and oxygen, lead and sulfur stable isotope data along with the geologic characteristics of the ore deposit it is believed that the oreforming solution was derived dominantly form meteoric water, while the ore-forming matirial was originated largely from the M rock body and the rest from the metasedimentary rocks. Genesis of the №376 uranium deposit is closely related to the Late-Caledonian metamorphism.
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【References】
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