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Uraniferous Black Shale and Related Uranium Mineralization Features in South ChinaOA

Uraniferous Black Shale and Related Uranium Mineralization Features in South China

中文摘要英文摘要

Black shales are marine sediments with argillaceous, silty and siliceous compositions and high contents of organic materials, disseminated pyrite and uranium. Uraniferous black shale has uranium content of more than 20 ppm. Black shales are widely distributed in 17 provinces or autonomous regions in northwestern and southern-central China. Their sedimentary ages are from the Sinian to the Tertiary and uraniferous black shales are mainly exposed in Yunnan, Guizhou, Sichuan, Hunan, Hubei, Jiangxi, and Zhejiang provinces and Guangxi Zhuang Autonomous Region and the economically significant uranium deposits associated with black shale occur in Hunan and Jiangxi provinces and Guangxi Zhuang Autonomous Region.Uranium mineralization associated with black shale has the following main features: (1) forming stratabound deposits; (2) controlled by structures such as interlayer and intersected faults and fractures; (3) associated with different ore-forming processes such as leaching and hydrothermal reworking; (4) occurring in five periods, namely 120- 110 Ma, 84- 74 Ma, 75- 65 Ma, 48- 39 Ma and 30- 24 Ma.

Black shales are marine sediments with argillaceous, silty and siliceous compositions and high contents of organic materials, disseminated pyrite and uranium. Uraniferous black shale has uranium content of more than 20 ppm. Black shales are widely distributed in 17 provinces or autonomous regions in northwestern and southern-central China. Their sedimentary ages are from the Sinian to the Tertiary and uraniferous black shales are mainly exposed in Yunnan, Guizhou, Sichuan, Hunan, Hubei, Jiangxi, and Zhejiang provinces and Guangxi Zhuang Autonomous Region and the economically significant uranium deposits associated with black shale occur in Hunan and Jiangxi provinces and Guangxi Zhuang Autonomous Region.Uranium mineralization associated with black shale has the following main features: (1) forming stratabound deposits; (2) controlled by structures such as interlayer and intersected faults and fractures; (3) associated with different ore-forming processes such as leaching and hydrothermal reworking; (4) occurring in five periods, namely 120- 110 Ma, 84- 74 Ma, 75- 65 Ma, 48- 39 Ma and 30- 24 Ma.

Bureau of Geology, China National Nuclear Corporation, P.O. Box 762, Beijing 100013

天文与地球科学

Uraniferous black shale;uranium mineralization features;leaching and hydrothermal reworking

Uraniferous black shale;uranium mineralization features;leaching and hydrothermal reworking

《地质学报(英文版)》 2000 (003)

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