河北唐山西部PZK14孔晚新生代沉积演化特征

doi:10.19388/j.zgdzdc.2022.03.07

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Abstract In order to find out the sedimentary evolution characteristics of loose deposits in the western plain of Tangshan since the Late Cenozoic, the authors in this paper studied the color, particle size, apparent resistivity logging and natural gamma logging of the borehole PZK14 in western Tangshan and divided the sedimentary facies with the calculation of deposition rate of each period , based on the 1∶50,000 regional geological survey in Yahongqiao area. The results show that lacustrine facies, delta facies and fluvial facies are mainly developed in this area during the Late Cenozoic. The delta facies was developed at the beginning of the Early Pleistocene, while the delta facies was transformed into fluvial facies with the retrogradation of alluvial fan in the ancient Luanhe River when the climate began to become warming. Three lake-delta sedimentary cycles developed during middle to late Early Pleistocene. A lake-delta sedimentary cycle developed in the Middle Pleistocene. At the beginning of Late Pleistocene, a thick lacustrine layer was deposited. As the climate became cold, the transgression along the coast of Bohai Bay ended and the lacustrine basin began to shrink and transformed into fluvial facies. The Holocene was dominated by interfluvial depression. According to the sedimentation rate-age curve, tectonic control of the sedimentation in this area has been weak since the Quaternary, and the climate is the main factor affecting the development of sedimentary facies. The sedimentation rate of the Quaternary was relatively fast, and the Olduvai polarity subchron (1.95~1.77 Ma) had the highest sedimentation rate of 194.0 m/Ma. The deposition rate of 2.52~1.95 Ma is the smallest, which is about 111.2 m/Ma. This achievement is of great significance to the restoration of paleogeographic evolution and the geological exploration of hydraulic environment in this region.

Key words： western Tangshan borehole sedimentary facies chroma grain size logging curves

Received: 13 January 2021

ZTFLH:	P56
	P586

Fund:中国地质调查局“河北1∶5万沙流河等四幅区域地质调查项目(编号: DD20160042-4)”; “特殊地质地貌区填图试点-河北1∶5万大厂回族自治县等三幅第四系覆盖区地质填图(编号: DD20160060)”; “河北海岸带区域地质资料汇编(编号: DD20179394)”; 河北地矿局“河北区域地质调查工作总结研究(编号: 201821)”项目联合资助

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	Articles by authors
	CHEN Hongqiang
	YANG Rui
	LI Qingzhe
	ZHAO Huaping
	DUAN Bingxin
	LIU Beibei
	ZHUAN Shaopeng
	CHEN Chao

Cite this article:

CHEN Hongqiang,YANG Rui,LI Qingzhe, et al. Sedimentary evolution of borehole PZK14 in western Tangshan area during Late Cenozoic[J]. , 2022, 9(3): 67-75.

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http://journal25.magtechjournal.com/Jwk_dzdc/EN/10.19388/j.zgdzdc.2022.03.07 OR http://journal25.magtechjournal.com/Jwk_dzdc/EN/Y2022/V9/I3/67

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