北京平原区南部PGZ01孔第四纪地层划分及其环境意义<sup>*</sup>

doi:10.7605/gdlxb.2018.02.025

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Abstract

Based on the core materials collected from the Borehole PGZ01,which is located at Yufa Township of Daxing district in southern Beijing plain area and has a depth of 420m,the analyses of lithostrotigraphy,magnetostratigraphy,AMS ¹⁴C dating,Ostracoda and sporopollen assemblages were carried out. The results show that: (1)The boundaries of Matuyama/Gauss polarity chron and Brunhes/Matuyama polarity chron appear at the depth of 280m and 78.35m, respectively. It suggests that the bottom strata of this borehole correspond to Gauss normal polarity zone at the bottom. Considering that the boundary of Matuyama/Gauss polarity chron at the depth of 280m is the lower boundary of Quaternary system. It suggests that the debris flow and alluvial fan or possible palaeo-Yongding River had arrived at the southern part of Beijing plain area before Quaternary. Moreover, thick-layer brownish red clay which is considered as the upper mark lithostratigraphic unit of the Pliocene occurred at the Olduvai subzone. (2)Integrated with the AMS ¹⁴C dating,the present study tentatively correlate the stratal oxidation-reduction status above the depth of 60m to correlate to cores from palaeomonsoonal-sensitive coastal plain environment,the boundary of the Upper Pleistocene and Holocene was determined to be at 56.60m and 18.95m, respectively. (3)The characteristic sediments deposited since MIS5 have a good correlation with core sediments from coastal plain environment,and show evidence of the influence of Prehistoric Flood of 8-4ka. The present paper provided important age control for subdividion and correlation of Quaternary stratigraphy,construction of palaeogeography,fault activities and tectonic history of the westnorthern margin region of Lang(fang)-Gu(an) Depression,and understanding of the environmental effect of palaeomonsoon change since the Late Pleistocene.

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	Articles by authors
	Zhao Yong
	Wang Qiang
	Li Rui-Jie
	Wei Bo
	Xu Ji-Xiang
	Sun Yong-Hua
	Zhang Xiao-Liang
	Wang Chun-Jun
	Zhou Yuan-Xin
	You Shi-Na
	Lv Jin-Bo

Key words： magnetostratigraphy Quaternary palaeo-Yongding River Beijing plain area

Received: 05 April 2016

ZTFLH:

P534.63

Fund:

[Co-funded by Beijing 1:50 000 Liulihe,Panggezhuang,Ancixian Regional Geological Survey Project of China Geological Survey(No. 12120114007701) and the National Natural Science Foundation of China(No. 40872107)]

Corresponding Authors: Wang Qiang,born in 1945,is a professor at Tianjin Geological Survey Centre. He is mainly engaged in Quaternary geology and marine geology. E-mail: tjwq1945@163.com.

About author: Zhao Yong,born in 1983,is a senior engineer at Beijing Institute of Geological Survey. He is mainly engaged in regional and Quaternary geology. E-mail: zhaoyong3068@163.com.About the corresponding author Wang Qiang,born in 1945,is a professor at Tianjin Geological Survey Centre. He is mainly engaged in Quaternary geology and marine geology. E-mail: tjwq1945@163.com.

Cite this article:

Zhao Yong,Wang Qiang,Li Rui-Jie et al. Quaternary stratigraphic division and its environmental significance of Borehole PGZ01 in southern Beijing plain area[J]. JOPC, 2018, 20(2): 337-348.

URL:

http://journal09.magtechjournal.com/gdlxb/EN/10.7605/gdlxb.2018.02.025 OR http://journal09.magtechjournal.com/gdlxb/EN/Y2018/V20/I2/337

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