洞庭盆地S3-7孔第四纪年代地层

赵举兴; 李长安; 张玉芬; 强小科; 熊德强

doi:10.3799/dqkx.2016.052

Volume 41 Issue 4

Apr. 2016

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Article Navigation > Earth Science > 2016 > 41(4): 633-643

Zhao Juxing, Li Chang'an, Zhang Yufen, Qiang Xiaoke, Xiong Deqiang, 2016. Quaternary Chronostratigraphy of Borehole S3-7 in Dongting Basin. Earth Science, 41(4): 633-643. doi: 10.3799/dqkx.2016.052

Citation:

Zhao Juxing, Li Chang'an, Zhang Yufen, Qiang Xiaoke, Xiong Deqiang, 2016. Quaternary Chronostratigraphy of Borehole S3-7 in Dongting Basin. Earth Science, 41(4): 633-643. doi: 10.3799/dqkx.2016.052

Zhao Juxing, Li Chang'an, Zhang Yufen, Qiang Xiaoke, Xiong Deqiang, 2016. Quaternary Chronostratigraphy of Borehole S3-7 in Dongting Basin. Earth Science, 41(4): 633-643. doi: 10.3799/dqkx.2016.052

Citation:

Zhao Juxing, Li Chang'an, Zhang Yufen, Qiang Xiaoke, Xiong Deqiang, 2016. Quaternary Chronostratigraphy of Borehole S3-7 in Dongting Basin. Earth Science, 41(4): 633-643. doi: 10.3799/dqkx.2016.052

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Quaternary Chronostratigraphy of Borehole S3-7 in Dongting Basin

doi: 10.3799/dqkx.2016.052

1.
School of Earth Sciences, China University of Geosciences, Wuhan 430074, China
2.
State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Wuhan 430074, China
3.
Institute of Geophysics & Geomatics, China University of Geosciences, Wuhan 430074, China
4.
State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences, Xi'an 710075, China

Received Date: 2015-09-29
Publish Date: 2016-04-15

Abstract

Abstract

The formation and evolution of the Dongting basin are important for understanding the geological environmental evolution of the middle Yangtze drainage and even central China. However, Quaternary chronostratigraphy is still controversial in the area. In this study, one continuous borehole S3-7 with a depth of 255.1 m was taken from the Yuanjiang depression, the deposition center of the Dongting basin. Based on detailed stratigraphic and lithological interpretations, the borehole was dated by paleomagnetism, ESR and AMS¹⁴C, to establish its chronostratigraphic sequence. Compared with other two typical boreholes, the Quaternary chronostratigraphic sequence of the Dongting basin was established. The results suggest that the Plio-Pleistocene and Early-Middle Pleistocene boundaries of the central Dongting basin are located at the depths of 240-300 m and 90-95 m, respectively, and the boundaries of Middle-Late Pleistocene and Pleistocene/Holocene are located at the depths of 28-50 m and 1.5-3.1 m, respectively. Average deposition rate and piecewise linear equation show that the timing of lithological units in coverage area are as follows: 2 590-1 600 ka BP for the Huatian Formation, 1 600-920 ka BP for the Xiangyin Formation, 920-120 ka BP for the Dongtinghu Formation, 120-11 ka BP for the Anxiang Formation and younger than 11 ka BP for the Holocene.
- Dongting basin,
- Quaternary,
- chronostratigraphy,
- paleomagnetism,
- geochronology,
- stratigraphy

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References(68)

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Quaternary Chronostratigraphy of Borehole S3-7 in Dongting Basin

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