Abstract
The methods following as field geological investigation, trace element geo- chemistry and isotope geochemistry were used in this project. Based on geological and geochemical characteristics of Xiaoshui uranium ore deposits in Zhongdong area, Xiazhuang ore-field, Guangdong province, it could be concluded that: (1) The Provenance of Cretaceous mantle is a enriched mantle; (2) Silicified zone-type and intersection-type uranium ore are distinctness in the metallogenic period and mineralization process, and main metallogenic period of Xiaoshui uranium ore-deposit is 73.5 Ma; (3) The sources of uranium mineralization substance derived from enriched mantle; and (4)The intersection-type high grade uranium deposits were controlled by substances derived from mantle (contain with U, CO{sub 2}, F, et al), tracks of intersection of NWW-across with NNE-trending faults and lithology of diabase. (authors)
Zhengqi, Wang;
[1]
Lieqin, Wu;
[2]
Guoyu, Zhang
[1]
- East China Inst. of Technology, Fuzhou (China)
- Institute No.290, CNNC, Shaoguan (China)
Citation Formats
Zhengqi, Wang, Lieqin, Wu, and Guoyu, Zhang.
Research on metallogenic conditions of intersection-type uranium ore-deposits in Zhongdong area, Northern Guangdong province.
China: N. p.,
2007.
Web.
Zhengqi, Wang, Lieqin, Wu, & Guoyu, Zhang.
Research on metallogenic conditions of intersection-type uranium ore-deposits in Zhongdong area, Northern Guangdong province.
China.
Zhengqi, Wang, Lieqin, Wu, and Guoyu, Zhang.
2007.
"Research on metallogenic conditions of intersection-type uranium ore-deposits in Zhongdong area, Northern Guangdong province."
China.
@misc{etde_21104131,
title = {Research on metallogenic conditions of intersection-type uranium ore-deposits in Zhongdong area, Northern Guangdong province}
author = {Zhengqi, Wang, Lieqin, Wu, and Guoyu, Zhang}
abstractNote = {The methods following as field geological investigation, trace element geo- chemistry and isotope geochemistry were used in this project. Based on geological and geochemical characteristics of Xiaoshui uranium ore deposits in Zhongdong area, Xiazhuang ore-field, Guangdong province, it could be concluded that: (1) The Provenance of Cretaceous mantle is a enriched mantle; (2) Silicified zone-type and intersection-type uranium ore are distinctness in the metallogenic period and mineralization process, and main metallogenic period of Xiaoshui uranium ore-deposit is 73.5 Ma; (3) The sources of uranium mineralization substance derived from enriched mantle; and (4)The intersection-type high grade uranium deposits were controlled by substances derived from mantle (contain with U, CO{sub 2}, F, et al), tracks of intersection of NWW-across with NNE-trending faults and lithology of diabase. (authors)}
place = {China}
year = {2007}
month = {Dec}
}
title = {Research on metallogenic conditions of intersection-type uranium ore-deposits in Zhongdong area, Northern Guangdong province}
author = {Zhengqi, Wang, Lieqin, Wu, and Guoyu, Zhang}
abstractNote = {The methods following as field geological investigation, trace element geo- chemistry and isotope geochemistry were used in this project. Based on geological and geochemical characteristics of Xiaoshui uranium ore deposits in Zhongdong area, Xiazhuang ore-field, Guangdong province, it could be concluded that: (1) The Provenance of Cretaceous mantle is a enriched mantle; (2) Silicified zone-type and intersection-type uranium ore are distinctness in the metallogenic period and mineralization process, and main metallogenic period of Xiaoshui uranium ore-deposit is 73.5 Ma; (3) The sources of uranium mineralization substance derived from enriched mantle; and (4)The intersection-type high grade uranium deposits were controlled by substances derived from mantle (contain with U, CO{sub 2}, F, et al), tracks of intersection of NWW-across with NNE-trending faults and lithology of diabase. (authors)}
place = {China}
year = {2007}
month = {Dec}
}