第四纪以来天津北部燕山隆升与山前盆地的形成<sup>*</sup>

doi:10.7605/gdlxb.2018.05.063

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Abstract

The present paper reported the integrated study on the sedimentology,stratigraphy,chronology,micropaleontology of four boreholes with high core recovery located on the piedmont zone of Yanshan Mountain in northern Tianjin. The inclination curve consisting of 420 hot demagnetizm samples from Borehole Z3 (unconsolidated deposits with 147 m thickness) indicated that the lower strata belong to the Matuyama polarity chron—dated at 2.58 Ma. Following the crustal subsidence,just from Early Pleistocene the mud sediments of alluvial fan fringe started packing the sediment space above the basal conglomerate layer in studied area,and fluvial plain formed in the generalized piedmont basin. Bright yellowish brown-yellow orange-bright reddish brown clay was continuously developed during middle Early Pleistocene. The regional subsidence center situated at the site from the piedmont fault less than 4 km at that time. The Brunhes polarity zone—dated 0.78 Ma is 57.8 m thick. On the basis of the fact that the bottom of Late Pleistocene had determined prudently based on the Blake subchron—dated 120 ka at Borehole Z3,it can be found that a larger part of Middle Pleistocene series absented. This feature is very like to the stratal hiatus found on the Cangxian Uplift in Tianjin area and in the south part of the Yongdinghe River fluvial plain in Beijing at the same time. A total of 7 ¹⁴C dating collecting from three boreholes confirmed that the thickest stratum since 45 ka has 40.7 m occurred at the borehole from the piedmont fault less than 2 km. It represents that under the tectonic fault effect since the initial period of MIS(Marine Isotope Stage)3,the subsidence center northward migrated to toe of the piedmont fault,a new narrow sense piedmont basin formed. In the study area, the earliest 15 ka organic-clay and overlaying peat occurred, suggesting that the warming since Last Deglacial stage had affected the piedmont area in the North China Plain firstly. The present study provided a datum mark for study on subsidence of west coastal plain of Bohai Bay in the source-to-sink processes since Late Cenozoic.

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	Sun Zhen-Ying
	Wang Qiang
	Li Ya-Ping
	Pei Jun-Ling
	Zhou Xiang-Guo
	Gao Xue-Fei

Key words： piedmont basin of Yanshan Mountain Magnetostrtigraphy ¹⁴C chronology uplift of Yanshan Mountain stratigraphic hiatus of Middle Pleistocene west coast of Bohai Bay source-to-sink

Received: 12 April 2018

ZTFLH:

P534.63

Fund:

National Natural Science Foundation of China(No.40872107)and the Project of the Quaternary Stratigraphic Texture of Jixian County of Tianjin(Tianjin Municipal Bureau of Land Resources and Housing Administration[2013]No.20)

Corresponding Authors: Wang Qiang,born in 1945,is a professor of Tianjin Center of Geological Survey,China Geological Survey and Key Laboratory of Muddy Coast Geo-Environment, China Geological Survey. He is mainly engaged in Quaternary geology and marine geology. E-mail: tjwq1945@163.com.

About author: Sun Zhen-Ying,born in 1963,is a senior engineer of City Geological Institute of Tianjin Municipality Survey Institute of Engineering Geology. He is mainly engaged in regional geology and Quaternary geology. E-mail: sunzhenying 1963@126.com.

Cite this article:

Sun Zhen-Ying,Wang Qiang,Li Ya-Ping et al. The uplift of Yanshan Mountain and the formation of piedmont basin in northern Tianjin since the Quaternary[J]. JOPC, 2018, 20(5): 893-908.

URL:

http://journal09.magtechjournal.com/gdlxb/EN/10.7605/gdlxb.2018.05.063 OR http://journal09.magtechjournal.com/gdlxb/EN/Y2018/V20/I5/893

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