利用滩坝砂体规模研究古风力的定量恢复<sup>*</sup>

doi:10.7605/gdlxb.2021.05.057

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Abstract

The strength of palaeowind,which is an important indicator for palaeoclimate,is difficult to be quantitatively reconstructed.The scale of wind-generated waves reflects wind strength,which may become a new idea for the reconstruction of palaeowind strength. The longshore bar and coastal bar that formed in the swash zone and surf backflow zone,can record wave breaking and swash processes,respectively. In this paper,the principal and workflow for reconstruction of palaeowave and palaeowind conditions by using longshore bar and coastal bar in ancient lakes were introduced. Two methods are used in this paper: (1)There is a functional relationship between the thickness of longshore bar and the water depth of breaking waves(i.e.,breaking depth)according to geometrical analysis. The breaking depth,in turn,is determined by breaking wave height. Thus the breaking wave height can be reconstructed by using ancient longshore bar thickness. The significant wave height and palaeowind strength can also be calculated according to empirical wind-wave relationship. Three parameters are required in this method: The thickness of the isolated longshore bar,the slope angle of the basement where the longshore bar sits,and the palaeo-fetch. (2)The thickness of coastal bar records the swash height,which is determined by significant wave height. The palaeowind strength can also be reconstructed according to empirical wind-wave relationship. Five parameters are required in the latter method: The original thickness of the isolated coastal bar,the average depth of the paleowater,the palaeofetch,the angle between the palaeowind direction and the normal to the shoreline,and the particle size. All these two integrated methods,which include the reconstruction of palaeowind direction,palaeoslope,palaeo-fetch,palaeo-water depth etc.,should apply techniques such as palaeogeomorphy,decompaction,location of the palaeoshoreline,reconstruction of palaeowater depth and the wave theory. Many beach-bar deposits are preserved in ancient lacustrine strata,which can be applied in the reconstruction of ancient wave regime and ancient wind regime. These can also be helpful in reconstruction of the palaeogeographic setting of the sedimentary basin.

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	Articles by authors
	Wang Jun-Hui
	Jiang Zai-Xing
	Xian Ben-Zhong
	Zhang Chun-Ming
	Li Guo-Bin

Key words： palaeowind palaeowave beach bar breaker zone swash zone single parameter sensitivity analysis

Received: 07 January 2021

ZTFLH:

P532

Fund:

Co-funded by the National Natural Science Foundation of China(Nos.41702104,41872113),National Science and Technology Major Project(No.2017ZX05009-002),and Science Foundation of China University of Petroleum(Beijing)(Nos.2462020BJRC002,2462020YXZZ020)

Corresponding Authors: Jiang Zai-Xing,born in 1962,is a professor and PhD supervisor of China University of Geosciences(Beijing).He is mainly engaged in sedimentology and sequence stratigraphy.E-mail: jiangzx@cugb.edu.cn.

About author: Wang Jun-Hui,born in 1988,is an associate professor of China University of Petroleum(Beijing).He is mainly engaged in sedimentology.E-mail: wangjunhui@cup.edu.cn.

Cite this article:

Wang Jun-Hui,Jiang Zai-Xing,Xian Ben-Zhong et al. Determination of palaeowind strength by using scale of beach-bar sand bodies[J]. JOPC, 2021, 23(5): 937-950.

URL:

http://journal09.magtechjournal.com/gdlxb/EN/10.7605/gdlxb.2021.05.057 OR http://journal09.magtechjournal.com/gdlxb/EN/Y2021/V23/I5/937

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