黔湘渝毗邻区南华纪武陵裂谷盆地结构及其对锰矿的控制作用

周琦; 杜远生; 袁良军; 张遂; 余文超; 杨胜堂; 刘雨

doi:10.3799/dqkx.2016.014

Volume 41 Issue 2

Feb. 2016

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Article Navigation > Earth Science > 2016 > 41(2): 177-188

Zhou Qi, Du Yuansheng, Yuan Liangjun, Zhang Sui, Yu Wenchao, Yang Shengtang, Liu Yu, 2016. The Structure of the Wuling Rift Basin and Its Control on the Manganese Deposit during the Nanhua Period in Guizhou-Hunan-Chongqing Border Area, South China. Earth Science, 41(2): 177-188. doi: 10.3799/dqkx.2016.014

Citation:

Zhou Qi, Du Yuansheng, Yuan Liangjun, Zhang Sui, Yu Wenchao, Yang Shengtang, Liu Yu, 2016. The Structure of the Wuling Rift Basin and Its Control on the Manganese Deposit during the Nanhua Period in Guizhou-Hunan-Chongqing Border Area, South China. Earth Science, 41(2): 177-188. doi: 10.3799/dqkx.2016.014

Citation:

Zhou Qi, Du Yuansheng, Yuan Liangjun, Zhang Sui, Yu Wenchao, Yang Shengtang, Liu Yu, 2016. The Structure of the Wuling Rift Basin and Its Control on the Manganese Deposit during the Nanhua Period in Guizhou-Hunan-Chongqing Border Area, South China. Earth Science, 41(2): 177-188. doi: 10.3799/dqkx.2016.014

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The Structure of the Wuling Rift Basin and Its Control on the Manganese Deposit during the Nanhua Period in Guizhou-Hunan-Chongqing Border Area, South China

doi: 10.3799/dqkx.2016.014

1.
103 Geological Party, Bureau of Geology and Mineral Exploration & Development of Guizhou Province, Tongren 554300, China
2.
Bureau of Geology and Mineral Exploration and Development of Guizhou Province, Guiyang 550004, China
3.
State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Wuhan 430074, China
4.
School of Earth Environment and Water Resource, Yangtze University, Wuhan 430100, China

Received Date: 2015-09-10
Publish Date: 2016-02-15

Abstract

Abstract

The "Datangpo type" manganese deposits in Guizhou-Hunan-Chongqing border area is an important manganese resource base since its hundreds of million tons of sedimentary rhodochrosite accounts for about half of manganese resource of China. In this paper, based on the study about the formation system of Nanhua period and stratigraphic regionalization, we find under the background of Rodinia supercontinent breakup, the Nanhua rift basin (level I) consisted of the Wuling and Xuefeng secondary rift basin and the Tianzhu-Huaihua uplift. Wuling secondary rift basin controlled and formed the manganese metallogenic area in the Guizhou-Hunan-Chongqing border area, and its inside consisted of three level Ⅲ depression basins, one level Ⅲ uplift and sixteen level IV rift basins. The three level Ⅲ depression basins controlled Songtao-Guzhang, Yiping-Zhijiang and Xikou-Xiaochayuan secondary manganese metallogenic area. Among them, the Songtao-Guzhang depression basin (Level Ⅲ) is the rifting center of the Wuling secondary rift basin, where the manganese mineralization is strong, and the quantity of resource is huge, which has became a world-level manganese concentrated area. The IV rift basins controlled and formed the manganese deposits in the target area. It's suggested that the syn-sedimentary fault in Nanhua period is the premise of manganese deposit formation, fifteen syn-sedimentary faults, the controlled depression basins and the major manganese in the target area are distinguished and recovered. The syn-sedimentary fault is not only the transporting tunnel of deep manganese material and ancient natural gas but also the link of inside system and surface system of ancient natural gas seepage sedimentary-type manganese metallogenic system.
- Nanhua period,
- rift basin,
- manganese deposit,
- South China,
- ore deposit geology

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References(64)

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The Structure of the Wuling Rift Basin and Its Control on the Manganese Deposit during the Nanhua Period in Guizhou-Hunan-Chongqing Border Area, South China

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