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Vertical grain-size trend of mouth bar in lacustrine fan delta:Flume experiments

Vertical grain-size trend of mouth bar in lacustrine fan delta: Flume experiments

作     者:Ke Zhang Sheng-He Wu Jun-Jie Wang Yun-Jie Xu Zhen-Hua Xu Jia-Jia Zhang 

作者机构:State Key Laboratory of Petroleum Resources and ProspectingChina University of Petroleum(Beijing)Beijing102249China College of GeosciencesChina University of Petroleum(Beijing)Beijing102249China School of GeosciencesYangtze UniversityWuhanHubei 430100China 

出 版 物:《Petroleum Science》 (石油科学(英文版))

年 卷 期:2022年第19卷第5期

页      面:1964-1977页

核心收录:

学科分类:081803[工学-地质工程] 08[工学] 0818[工学-地质资源与地质工程] 

基  金:supported by the National Natural Science Foundation of China(No.41772101) 

主  题:Mouth bar Vertical grain-size trend Effluent behavior Inertia Bed friction 

摘      要:Field observational previously indicated a mouth bar of a fan delta could exhibit a fining-or coarseningupward trend,which bring a new challenge to the identification of mouth bar in subsurface studies due to the lack of morphological *** studies have indicated that effluent behavior in rivermouth system can affect the vertical grain-size trend of mouth bar,but the drivers and magnitude of this phenomenon are not *** conducted flume experiments to investigate the mechanism and controlling factors of vertical grain-size trend of mouth *** with a steeper slope of the substrate layer,greater discharge,higher sediment/water ratio,and coarser sediment induced a finingupward trend of mouth bar,because the effluent was dominated by strong *** bar in the experiment with a gentler slope of the substrate layer,smaller discharge,lower sediment/water ratio,and finer sediment exhibited a coarsening-upward trend dominated by the friction-dominated *** relationship between the vertical grain-size trend of mouth bar and the gradients of foreset bedding in small-scale flume models and the cut-off of 15°-18°are applicable in natural *** depositional setting to infer depositional process in river-mouth system and analyzing the plane geometry of sandbodies are two steps in the interpretation of ancient fan deltaic rock record.

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