湘中地区南华系沉积序列、物源特征及区域对比

宋芳; 牛志军; 何垚砚; 杨文强

doi:10.3799/dqkx.2019.065

Volume 44 Issue 9

Sep. 2019

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Article Navigation > Earth Science > 2019 > 44(9): 3074-3087

Song Fang, Niu Zhijun, He Yaoyan, Yang Wenqiang, 2019. Sedimentary Sequence, Provenance and Stratigraphic Correlation of Nanhuan System in Middle Hunan Province. Earth Science, 44(9): 3074-3087. doi: 10.3799/dqkx.2019.065

Citation:

Song Fang, Niu Zhijun, He Yaoyan, Yang Wenqiang, 2019. Sedimentary Sequence, Provenance and Stratigraphic Correlation of Nanhuan System in Middle Hunan Province. Earth Science, 44(9): 3074-3087. doi: 10.3799/dqkx.2019.065

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Sedimentary Sequence, Provenance and Stratigraphic Correlation of Nanhuan System in Middle Hunan Province

doi: 10.3799/dqkx.2019.065

Song Fang^{1,2,3
,},
Niu Zhijun^1,3,
He Yaoyan^2,3,
Yang Wenqiang^1,3

1.
Wuhan Center of China Geological Survey, Wuhan 430205, China
2.
Institute of Geological Survey, China University of Geosciences, Wuhan 430074, China
3.
Key Laboratory of Paleontology and Coevolution of Life and Environment, China Geological Survey, Wuhan 430205, China

Received Date: 2018-11-23
Publish Date: 2019-09-15

Abstract

Abstract

During the Late Neoproterozoic, the Middle Hunan Province was located in the Yangtze platform marginal basin, making the deposits of this area as key for stratigraphic correlations. By the sedimentary measurement of Caihuatian section in Ningxiang and Majindong sections in Taoyuan, the sequence of Nanhuan System in the Middle Hunan is defined as Changan, Fulu (Gucheng included in some areas), Datangpo and Nantuo/Hongjiang formations. And to the north of Caihuatian section, no Changan Formation has been recognized. One detrital zircon sample from the lower part of Changan Formation of Caihuatian section shows the Yangtze provenance and 752.5±4.2 Ma (n=3, MSWD=2.4) deposition age. On the basis of sedimentary characteristics and research results in the area, the Changan Glaciation might be the correspondence of the bottom part of Sturtian Glaciation (760 Ma) and Changan and Fulu (Gucheng included) formations could correspond to the whole Sturtian Glaciation with different glacial deposition phases for diverse and periodical glacier in the area. Datangpo Formation was deposited in warm climate and Nantuo/Hongjiang Formation corresponded to Marinoan. Further research should be done to identify the correlation to strata below Datangpo Formation.
- Middle Hunan Province,
- Nanhuan System,
- sedimentary sequence,
- provenance,
- detrital zircon,
- stratigraphy

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Sedimentary Sequence, Provenance and Stratigraphic Correlation of Nanhuan System in Middle Hunan Province

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