黔东松桃南华系大塘坡组锰矿层物源：来自Sr同位素的证据

余文超; 杜远生; 周琦; 彭头平; 王萍; 袁良军; 徐源; 潘文; 谢小峰; 齐靓

doi:10.3799/dqkx.2016.092

Volume 41 Issue 7

Jul. 2016

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Article Navigation > Earth Science > 2016 > 41(7): 1110-1120

Yu Wenchao, Du Yuansheng, Zhou Qi, Peng Touping, Wang Ping, Yuan Liangjun, Xu Yuan, Pan Wen, Xie Xiaofeng, Qi Liang, 2016. Provenance of Nanhuan Datangpo Formation Manganese Mn Deposit in Songtao Area, East Guizhou Province: Evidence from Sr Isotope. Earth Science, 41(7): 1110-1120. doi: 10.3799/dqkx.2016.092

Citation:

Yu Wenchao, Du Yuansheng, Zhou Qi, Peng Touping, Wang Ping, Yuan Liangjun, Xu Yuan, Pan Wen, Xie Xiaofeng, Qi Liang, 2016. Provenance of Nanhuan Datangpo Formation Manganese Mn Deposit in Songtao Area, East Guizhou Province: Evidence from Sr Isotope. Earth Science, 41(7): 1110-1120. doi: 10.3799/dqkx.2016.092

Citation:

Yu Wenchao, Du Yuansheng, Zhou Qi, Peng Touping, Wang Ping, Yuan Liangjun, Xu Yuan, Pan Wen, Xie Xiaofeng, Qi Liang, 2016. Provenance of Nanhuan Datangpo Formation Manganese Mn Deposit in Songtao Area, East Guizhou Province: Evidence from Sr Isotope. Earth Science, 41(7): 1110-1120. doi: 10.3799/dqkx.2016.092

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Provenance of Nanhuan Datangpo Formation Manganese Mn Deposit in Songtao Area, East Guizhou Province: Evidence from Sr Isotope

doi: 10.3799/dqkx.2016.092

1.
State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Wuhan 430074, China
2.
Bureau of Geology and Mineral Exploration and Development of Guizhou Province, Guiyang 550004, China
3.
Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, China
4.
103 Geological Party, Bureau of Geology and Mineral Exploration and Development of Guizhou Province, Tongren 554300, China

Received Date: 2015-08-21
Publish Date: 2016-07-15

Abstract

Abstract

Provenance of manganese deposit is a key problem in the manganese metallogenic study. For a better understanding on the metallogenic process of the Nanhuan manganese deposit in Songtao area, East Guizhou Province, we need to gain a clear idea of the provenance of this manganese deposit. The Sr isotope study on the Mn deposit in Lower Nanhuan Datangpo Formation in Songtao, East Guizhou Province indicates that ⁸⁷Sr/⁸⁶Sr ratios in 15 samples vary in 0.705 727-0.732 536. Studied samples include Mn ore, Mn shale and black shale in the Mn-bearing layer and the highest ⁸⁷Sr/⁸⁶Sr ratio appears in the black shale sample. With Al (%) increasing in samples, ⁸⁷Sr/⁸⁶Sr ratios show two changing trends: the rising trend indicates terrigenous materials input and the falling trend indicates the deep hydrothermal sources input. As to ⁸⁷Sr/⁸⁶Sr ratios via Mn (%), there is no significant correlation coefficient, but ⁸⁷Sr/⁸⁶Sr ratios decrease when Mn (%) increase generally, according to residual analysis, we find that this is caused by the convergence fluctuation of ⁸⁷Sr/⁸⁶Sr ratios against the Mn(%) changes. The broad variation of ⁸⁷Sr/⁸⁶Sr ratios in Mn layer is caused by the dual inputs from terrigenous materials and hydrothermal sources. Compared with the contemporary (about 660 Ma)Sr isotope ratio in paleoseawater and the Sr isotope data from different ages Mn deposit world wide, we find that the broad variation of ⁸⁷Sr/⁸⁶Sr ratios in the Datangpo Formation. Mn layer does not conform to the feature of hydrogenetic Mn deposit. Considered with the specific geological background, we believe that the accumulation and precipitation of manganese are separated processes:the accumulation of Mn had finished in the anoxic basin during the Sturtian glaciation, whereas the Mn deposit precipitated in an unstable paleoceanographic environment at the beginning of interglaciation.
- Sr isotope,
- Datangpo Formation,
- Mn deposit,
- provenance,
- Guizhou Province,
- mineral geology

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References(76)

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Provenance of Nanhuan Datangpo Formation Manganese Mn Deposit in Songtao Area, East Guizhou Province: Evidence from Sr Isotope

doi: 10.3799/dqkx.2016.092

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通讯作者: 陈斌, bchen63@163.com

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