Research progresses of the genetic mechanism and architecture characterization on lake bars
Qiu Long-Wei1,2, Li Xin1, Yang Yong-Qiang1,2, Dong Dao-Tao1, Fu Jian1, Wen Xu1, Danish Khan1
1 School of Geosciences,China University of Petroleum(East China),Shandong Qingdao 266580,China; 2 Key Laboratory of Oil and Gas,Shandong Qingdao 266580,China
Abstract：Due to the repeated washing of waves and longshore currents,the bar reservoir has a high maturity,showing great oil and gas exploration potential,and has become the focus of subtle oil and gas reservoir exploration. Based on literature review,we summarize the recent research progresses of bar definitions,sedimentary characteristics,main controlling factors,genetic mechanisms and internal architectures,and propose a new understanding of bar evolution stage and sedimentary architecture. The results show that the bar evolution mainly includes weak wave action stage,turbulent current swash-backwash stage,aeolian stage and swampiness stage. Many factors affect the bar development,in which provenance is the clasts supplier and wind field is the energy engine. Hydrodynamic force induced by the wind strongly affects the development of bar reservoirs. Tectonic movement and sequence evolution control the distribution position and preservation of the bar. The above-mentioned factors work together to determine the morphology,scale,and preservation of the bar. According to the architectural theories,bar architecture is divided into six levels. In this architecture classification,we define composite sand body as level 5,single sand body as level 4 and accretive body as level 3,which are in reservoir scale. We explore the qualitative and quantitative characterization of the bar architecture level 3 to level 5 to provide theoretical support for beach-bar reservoir exploration and development.
Qiu Long-Wei,Li Xin,Yang Yong-Qiang et al. Research progresses of the genetic mechanism and architecture characterization on lake bars[J]. JOPC, 2022, 24(2): 191-209.
[1] 白立科,邱隆伟,杨勇强,杜双虎,杨保良,韩晓彤. 2020. 山东峡山湖东岸现代滩坝沉积模式及控制因素. 古地理学报, 22(2): 278-294. [Bai L K,Qiu L W,Yang Y Q,Du S H,Yang B L,Han X T. 2020. Sedimentary model and controlling factors of modern beach-bar sediments in east coast of Xiashan Lake in Shandong Province. Journal of Palaeogeography(Chinese Edition), 22(2): 278-294] [2] 操应长,王艳忠,徐涛玉,刘惠民,高永进. 2009. 东营凹陷西部沙四上亚段滩坝砂体有效储层的物性下限及控制因素. 沉积学报, 27(2): 230-237. [Cao Y C,Wang Y Z,Xu T Y,Liu H M,Gao Y J. 2009. The petrophysical parameter cutoff and controlling factors of the effective reservoir of beach and bar sandbodies of the upper part of the fourth member of the Shahejie formation in west part of Dongying depression. Acta sedimentological sinica, 27(2): 230-237] [3] 操应长,杨田,王健,远光辉,葸克来,李晓艳. 2013. 东营凹陷南坡沙四上亚段滩坝砂岩有效储层成因. 中国石油大学学报(自然科学版), 37(6): 1-9. [Cao Y C,Yang T,Wang J,Yuan G H,Xi K L,Li X Y. 2013. Genesis of effective reservoirs of beach-bar sandstone inupper part of the fourth member of Shahejie formationin the southern slope of Dongying sag. Journal of China University of Petroleum, 37(6): 1-9] [4] 陈彬滔,史忠生,马凤良,何巍巍,薛罗,马轮,贾义蓉. 2018. 南苏丹Melut盆地Ruman凹陷白垩系层序地层级次与砂质滩坝的沉积响应. 古地理学报, 20(6): 1013-1022. [Chen B T,Shi Z S,Ma F L,He W W,Xue L,Ma L,Jia Y R. 2018. Cretaceous sequence stratigraphic hierachies and the sedimentary response of sandy beach-bar in Ruman sag,Melut Basin,South Sudan. Journal of Palaeogeography(Chinese Edition), 20(6): 1013-1022] [5] 陈启林,黎瑞,金振奎,彭飚,朱小二,袁坤,王菁. 2019. 青海湖滩坝分布规律及其古气候意义. 现代地质,33(1): 187-197. [Chen Q L,Li R,Jin Z K,Peng B,Zhu X E,Yuan K,Wang J. 2019. Beach bar distribution and paleoclimate implications in Qinghai Lake. Geoscience, 33(1): 187-197] [6] 陈世悦,杨剑萍,操应长. 2000. 惠民凹陷西部下第三系沙河街组两种滩坝沉积特征. 煤田地质与勘探,(3): 1-4. [Chen S Y,Yang J P,Cao Y C. 2000. Sedimentary characteristics of two kinds of beach dams in the lower Tertiary Shahejie Formation in the west of Huimin Depression. Coal Geology & Exploration,(3): 1-4] [7] 高亮,孙波,王延章. 2018. 渤海湾盆地东营凹陷南坡沙四上亚段滩坝沉积特征及控制因素. 石油实验地质,40(5): 669-675. [Gao L,Sun B,Wang Y Z. 2018. Sedimentary characteristics and controlling factors of beach-bar sandstones of the upper section of the fourth member of Shahejie Formation on the southern slope of Dongying Sag,Bohai Bay Basin. Petroleum Geology & Experiment, 40(5): 669-675] [8] 郭晓,巨恳,戴越,袁青春. 2017. 纯化油田湖相滩坝薄储层含油性差异及控制因素. 山东国土资源, 33(10): 39-45. [Guo X,Ju k,Dai Y,Yuan Q C. 2017. Differences and controlling factors of oil-bearing in thin reservoir of lake facies beach-bar in Chunhua Oilfield. Shandong Land and Resources, 33(10): 39-45] [9] 范竹清. 2009. 东营凹陷滩坝油藏地球化学研究. 中国地质大学(北京)硕士论文: 1-52. [Fan Z Q. 2019. Geochemical study on beach bar reservoirs in Dongying Depression. Masteral dissertation of China University of Geosciences(Beijing): 1-52.] [10] 韩元红,郝乐伟,王琪,陆建林,朱建辉,罗厚勇. 2016. 青海湖近岸现代沉积滩坝主要类型及沉积特征. 古地理学报, 18(5): 759-768. [Han Y H,Hao L W,Wang Q,Lu J L,Zhu J H,Luo H Y. 2016. Sedimentary characteristics and types of beach bars deposited in modern times in nearshore of Qinghai Lake. Journal of Palaeogeography(Chinese Edition), 18(5): 759-768] [11] 何敏,汤军,刘一慧,廖春,柳誉剑. 2013. 柴达木盆地油砂山油田滩坝储集体沉积特征与非均质性研究. 天然气勘探与开发, 36(4): 17-21,6. [He M,Tang J,Liu Y H,Liao C,Liu Y J. 2013. Sedimentary features and heterogeneity of beach-bar reservoir body in Youshashan Oilfield,Qaidam Basin. Natural Gas Exploration and Development, 36(4): 17-21,6] [12] 胡晨林,张元福,姜在兴,王敏,高勇,白一鸣. 2015. 风浪作用下鄱阳湖现代滨岸滩坝的形态变化. 石油学报, 36(12): 1543-1552. [Hu C L,Zhang Y F,Jiang Z X,Wang M,Gao Y,Bai Y M. 2015. Morphologic changes in modern onshore beach bar of Poyang lake under wind and wave actions. Acta Petrolei Sinica, 36(12): 1543-1552] [13] 黄道军,钟寿康,张道锋,王保保,廖建初,谢康,卢子兴,谭秀成. 2021. 蒸发背景沉积序列精细刻画及沉积学解译: 以鄂尔多斯盆地中部中奥陶统马五6亚段为例. 古地理学报, 23(4): 735-755. [Huang D J,Zhong S K,Zhang D F,Wang B B,Liao J C,Xie K,Lu Z X,Tan X C. 2021. Datailed characterization and interpretation of sedimentary sequencesunder evaporitic environments: a case from the Ma56 submember of Middle Ordovician in central Ordos Basin. Journal of Palaeogeography(Chinese Edition), 23(4): 735-755] [14] 姜在兴,王俊辉,张元福. 2015. 滩坝沉积研究进展综述. 古地理学报, 17(4): 427-440. [Jiang Z X,Wang J H,Zhang Y F. 2015. Advances in beach-bar research: A review. Journal of Palaeogeography(Chinese Edition), 17(4): 427-440] [15] 姜在兴,王俊辉,张元福,张建国,宋明水,王玉华,姜洪福. 2020. “风—源—盆”三元耦合油气储集体预测方法及其应用: 对非主力物源区储集体的解释与预测. 石油学报, 41(12): 1465-1476. [Jiang Z X,Wang J H,Zhang Y F,Zhang J G,Song M S,Wang Y H,Jiang H F. 2020. Ternary “Windfield-Source-Basin”system for the prediction of hydrocarbon reservoirs: interpretation and prediction of hydrocarbon reservoirs deviated from the main provenance areas. Acta petrolei sinica, 41(12): 1465-1476] [16] 李维禄. 2016. 塔里木盆地东河砂岩体储层构型成因模式研究. 中国石油大学(北京)博士论文: 1-148. [Li W L. 2016. Genetic model of the reservoir architecture within the Donghe sandstones in Tarim Basin. Docteral dissertation of China University of Petroleum(Beijing): 1-148] [17] 林会喜,邓宏文,秦雁群,高晓鹏,龙国清,赵宁,颜晖,潘福友,邸永香. 2010. 层序演化对滩坝储集层成藏要素与分布的控制作用. 石油勘探与开发, 37(6): 680-689. [Lin H X,Deng H W,Qin Y Q,Gao X P,Long G Q,Zhao N,Yan H,Pan F Y,Di Y X. 2010. Control of sequence stratigraphic evolution on the distribution and hydrocarbon accumulation of beach and bar reservoirs. Petroleum Exploration and Development, 37(6): 680-689] [18] 龙明,徐怀民,江同文,牛玉杰,徐朝晖,陈玉琨. 2012. 滨岸相碎屑岩储集层构型动态评价. 石油勘探与开发, 39(6): 754-763. [Long M,Xu H M,Jiang T W,Niu Y J,Xu C H,Chen Y K. 2012. Performance evaluation for littoral-facies clastic reservoir architecture. Petroleum Exploration and Development, 39(6): 754-763] [19] 鹿坤. 2009. 济阳坳陷滩坝油藏成藏体系研究. 中国地质大学(北京)博士论文: 1-124 [Lu K. 2009. Study on hydrocarbon accumulation of beach bar reservoirs in Jiyang Depression. Docteral dissertation of China University of Geosciences(Beijing): 1-124] [20] 路顺行. 2008. 大王北地区沙二段高频层序与滩坝储层研究. 中国海洋大学博士论文: 1-78. [Lu S X. 2008. Research of Es2 high resolution sequence strata and beach-dam sandstone in the Dawangbei area. Docteral dissertation of Ocean University of China: 1-78] [21] 彭伟. 2019. 江汉盆地新沟嘴组下段滩坝砂沉积及分布特征. 长江大学学报(自然科学版),16(3):9-15,14-15. [Peng W. 2019. The sedimentation and distribution characteristics of beach-bar sand in the lower section of Xinguozui Formation in Jianghan Basin. Journal of Yangtze University(Natural Science Edition), 16(3):9-15,4-5] [22] 商晓飞,侯加根,孙福亭,唐力,刘钰铭,李永强,李燕. 2014. 砂质滩坝储集层内部结构特征及构型模式: 以黄骅坳陷板桥油田古近系沙河街组为例. 石油学报, 35(6): 1160-1171. [Shang X F,Hou J G,Su F T,Tang L,Liu Y M,Li Y Q,Li Y. 2014. Architectural characteristics and sedimentary models of beach-bar sandstone reservoirs: a case study of the Paleogene Shahejie Formation in Banqiao oilfield,Huanghua depression. Acta Sedimentologica Sinica, 35(6): 1160-1171] [23] 商晓飞,郭颖,侯加根,段太忠,赵磊. 2018. 湖泊滨岸砂坝内部结构特征剖析及其地质意义: 以峡山湖现代砂坝沉积为例. 沉积学报, 36(5): 877-889. [Shang X F,Guo Y,Hou J G,Duan T Z,Zhao L. 2018. Anatomy of architecture characteristics in lacustrine sand banks and its geological implications: a case study of modern sand banks in XiashanLake. Acta sedimentological sinica, 36(5): 877-889] [24] 宋春晖,方小敏,师永民,王新民. 2000. 青海湖西岸风成沙丘特征及成因. 中国沙漠,(4): 99-102. [Song C H,Fang X M,Shi Y M,Wang X M. 2000. Characteristics and genesis of Eolian Sand Dunes on the west coast of Qinghai Lake. Journal of Desert Research,(4): 99-102] [25] 唐武,仲米虹,田建华,邹梦君. 2015. 塔北地区黄山街组湖盆滩坝砂体沉积模式. 新疆石油地质, 36(3): 299-303. [Tang W,Zhong M H,Tian J H,Zou M H. 2015. Depositional model for lacustrine beach bars of Huangshanjie Formation in Tabei Area,Tarim Basin. Xinjiang Petroleum Geology, 36(3): 299-303] [26] 王冠民,王群,王春阳,付尧. 2016. 论湖相滩与坝的成因差异. 吉林大学学报(地球科学版), 46(1): 1-10. [Wang G M,Wang Q,Wang C Y,Fu Y. 2016. Discussion on genesis difference of lake beach and bar. Journal of Jilin University(Earth Science Edition), 46(1): 1-10] [27] 王菁,李相博,刘化清,张志杰,完颜容,王宏波,黄军平. 2019. 陆相盆地滩坝砂体沉积特征及其形成与保存条件: 以青海湖现代沉积为例. 沉积学报, 37(5): 1016-1030. [Wang J,Li X B,Liu H Q,Zhang Z J,Wan Y R,Wang H B,Huang J P. 2019. Sedimentary characteristics and conditions of formation and preservation of beach bar sand body in continental basin: taking modern sedimentation of Qinghai Lake as an example. Acta Sedimentologica Sinica, 37(5): 1016-1030] [28] 王俊辉,姜在兴,鲜本忠,张春明,李国斌. 2021. 利用滩坝砂体规模研究古风力的定量恢复. 古地理学报, 23(5): 937-950. [Wang J H,Jiang Z X,Xian B Z,Zhang C M,Li G B. 2021. Determination of palaeowind strength by using scale of beach-bar sand bodies. Journal of Palaeogeography(Chinese Edition), 23(5): 937-950] [29] 王腾飞,金振奎,Aliyeva G,王金艺,黎瑞,袁坤. 2018. 湖盆滩坝沉积研究进展. 科技导报, 36(23): 57-67. [Wang T F,Jin Z K,Aliyeva G,Wang J Y,Li R,Yuan K. 2018. Research progress of beach and dam deposition in lake basin. Seience and Technology innovation Herald, 36(23): 57-67] [30] 王夏斌,姜在兴,胡光义,范廷恩,王俊辉,卢欢. 2019. 辽河盆地西部凹陷古近系沙四上亚段沉积相及演化. 吉林大学学报(地球科学版), 49(5): 1222-1234. [Wang X B,Jiang Z X,Hu G Y,Fan T E,Wang J H,Lu H. 2019. Sedimentary facies and evolution of upper Fourth Member of Paleogene Shahejie Formation in western sag of Liaohe Basin. Journal of Jilin University(Earth Scicnce Edition), 49(5): 1222-1234] [31] 王旭影,姜在兴. 2020. 苏北盆地古近系阜三段沉积体系特征与模式. 现代地质, 34(6): 1132-1143. [Wang X Y,Jiang Z X. 2000. Sedimentary characteristics and mode of the Paleogene Funing formation(3rd Member)in the Subei Basin. Geoscience, 34(6): 1132-1143] [32] 王延章,宋国奇,王新征,陈建平,肖淑明. 2011. 古地貌对不同类型滩坝沉积的控制作用: 以东营凹陷东部南坡地区为例. 油气地质与采收率, 18(4): 13-16,111-112. [Wang Y Z,Song G Q,Wang X Z,Chen J P,Xiao S M. 2011. The controlling effect of paleogeomorphology on different types of beach and dam deposition: a case study of the south slope area in the east of Dongying Depression. Petroleum Geology and Recovery Efficiency, 18(4): 13-16,111-112] [33] 王永诗,高阳,方正伟. 2021. 济阳坳陷古近系致密储集层孔喉结构特征与分类评价. 石油勘探与开发, 48(2): 266-278. [Wang Y S,Gao Y,Fang Z W. 2021. Pore throat structure and classification of Paleogene tight reservoirs in Jiyang depression,Bohai Bay Basin,China. Petroleum Exploration and Development, 48(2): 266-278] [34] 魏恒飞,关平,王鹏,吴颜雄,李秋媛. 2019. 柴达木盆地滩坝沉积特征、成因及沉积模式: 以扎哈泉地区上干柴沟组为例. 高校地质学报, 25(4): 568-577. [Wei H F,Guan P,Wang P,Wu Y X,Li Q Y. 2019. Sedimentary characteristics,origin,and model of beach-bar in the Qaidam Basin: a case of the upper Ganchaigou formation in the Zhahaquan area. Geological journal of China Universities, 25(4): 568-577] [35] 吴崇筠,刘宝珺,王德发,信荃麟,项立嵩. 1981. 碎屑岩沉积相模式. 石油学报, 2(4): 1-10. [Wu C Y,Liu B J,Wang D F,Xin Q L,Xiang L S. 1981. Depositional facies model of clastic rocks. Acta Petrolei Sinica, 2(4): 1-10] [36] 吴胜和,纪友亮,岳大力,印森林. 2013. 碎屑沉积地质体构型分级方案探讨. 高校地质学报, 19(1): 12-22. [Wu S H,Ji Y L,Yue D L,Yin S L. 2013. Discussion on hierarchical scheme of architectural units in clastic deposits. Geological Journal of China Universities, 19(1): 12-22] [37] 吴小斌,侯加根,王大兴,滑双君,李树庆,吴辉,高星星. 2014. 黄骅坳陷港中油田滩坝砂单一坝精细解剖. 矿物岩石, 34(3): 89-97. [Wu X B,Hou J G,Wang D X,Hua S J,Li S Q,Wu H,Gao X X. 2014. Research of single bar dissection of beach-bar sand of the Gangzhong oil field in Huanghua depression. Mineralogy and Petrology, 34(3): 89-97] [38] 夏晓敏,吴颜雄,张审琴,薛建勤,王岚,施奇,崔涵,赵权. 2019. 湖相滩坝砂体构型及对致密油甜点开发的意义: 以柴达木盆地扎哈泉地区扎2井区为例. 天然气地球科学, 30(8): 1158-1167. [Xia X M,Wu Y X,Zhang S Q,Xue J Q,Wang L,Shi Q,Cui H,Zhao Q. 2019. Study on sand body architecture of lacustrine beach-bar and significance for development of tight oil sweet areas: a case study of Well Za-2 area in Zahaquan area,Qaidam Basin. Natural Gas Geoscience, 30(8): 1158-1167] [39] 肖波. 2017. 大王庄地区沙二段层序地层特征与滩坝发育的关系. 矿物岩石, 37(3): 55-60. [Xiao B. 2017. Relationship between sequence stratigraphic characteristics and development of beach bars in the second member of Shahejie formation in Dawangzhuang area. Mineralogy and Petrology, 37(3): 55-60] [40] 杨萍. 2011. 青海湖的形成与环境演化. 青海环境, 21(2): 59-61,75. [Yang P. 2011. The formation and evolution of Qinghai Lake. Journal of Qinghai Environment, 21(2): 59-61,75] [41] 杨勇强,邱隆伟,姜在兴,银熙炉. 2011. 陆相断陷湖盆滩坝沉积模式: 以东营凹陷古近系沙四上亚段为例. 石油学报, 32(3): 417-423. [Yang Y Q,Qiu L W,Jiang Z X,Yin X L. 2011. A depositional pattern of beach bar in continental rift lake basins: a case study on the upper part of the fourth member of the Shahejie Formation in the Dongying Sag. Acta Petrolei Sinica, 32(3): 417-423] [42] 袁坤,金振奎,彭飚,朱小二,田甜,黎瑞. 2020青海湖东南岸现代滩坝沉积模式与识别标志. 现代地质, 34(2): 309-320. [Yuan K,Jin Z K,Peng B,Zhu X E,Tian T,Li R. 2020. Sedimentary model and identification marks of modern macustrine beach-bar on southeast coast of Qinghai Lake. Geoscience, 34(2): 309-320] [43] 张天舒,陶士振,吴因业,杨家静,庞正炼,杨晓萍,陈燕燕,袁苗,刘敏,范建玮,冯荣昌. 2019. 层序演化对三角洲—滩坝沉积体系有利储层类型与分布的控制作用: 以四川盆地中部侏罗系凉高山组为例. 天然气地球科学, 30(9): 1286-1300. [Zhang T S,Tao S Z,Wu Y Y,Yang J J,Pang Z L,Yang X P,Chen Y Y,Yuan M,Liu M,Fan J W,Feng R C. 2019. Control of sequence stratigraphic evolution on the types and distribution of favorable reservoir in the delta and beach-bar sedimentary system: Case study of Jurassic Lianggaoshan Formation in Central Sichuan Basin. Natural Gas Geoscience, 30(9): 1286-1300] [44] 周清波,舒誉,朱筱敏,陈兆明,董小云,林秋金. 2019. 珠江口盆地HA地区古近系文昌组沉积特征. 高校地质学报, 25(4): 558-567. [Zhou Q B,Shu Y,Zhu X M,Chen Z M,Dong X Y,Lin Q J. 2019. Sedimentary Characteristics of the Paleogene Wenchang Formation in the HA Area,Pearl River Mouth Basin. Geological Journal of China Universities, 25(4): 558-567] [45] 朱筱敏,信荃麟,张晋仁. 1994. 断陷湖盆滩坝储集体沉积特征及沉积模式. 沉积学报, 12(2): 20-28. [Zhu X M,Xin Q L,Zhang J R. 1994. The sedimentary characteristics and model of the reservoir collective in the beach-bar basin of the fault depression. Acta Sedimentologica Sinica, 12(2): 20-28] [46] 邹才能,赵文智,张兴阳,罗平,王岚,刘柳红,薛叔浩,袁选俊,朱如凯,陶士振. 2008. 大型敞流坳陷湖盆浅水三角洲与湖盆中心砂体的形成与分布. 地质学报, 82(6): 813-825. [Zou C N,Zhao W Z,Zhang X Y,Luo P,Wang L,Liu L L,Xue S H,Yuan X J,Zhu R K,Tao S Z. 2008. Formation anddistribution of shallow water deltas and central basin sandbodies inlarge open depression lake basins. Acta Gologica Sinica, 82(6): 813-825] [47] An Z S,Wang P,Shen J,Zhuang Y X,Zhang P Z,Wang S M,Li X Q,Sun Q L,Song Y G,Ai L,Zhang Y C,Jiang S R Liu X Q,Wang Y. 2006. Geophysical survey on the tectonic and sediment distribution of Qinghai Lake basin. Science in China: Series D Earth Sciences, 49(8): 851-861. [48] An Z S,Wu G X,Li J P,Sun Y B,Liu Y M,Zhou W J,Cai Y J,Duan A M,Li L,Mao J Y,Cheng H,Shi Z G,Tan L C,Yan H,Ao H,Chang H,Feng J. 2015. Global monsoon dynamics and climate change. Annual Review of Earth and Planetary Sciences, 43: 29-77. [49] Campbell V C. 1971. Depositional model-upper cretaceous Gallup Beachshor Eline,ship rock area,Northwestern New-Mexico. Journal of Sedimentary Research, 41(2): 395-409. [50] Clems C D,Pitts A,Jablonska D,Haynes J T. 2020. Backset lamination produced by supercritical backwash flows at the beachface-shoreface transition of a storm-dominated gravelly beach(middle Pleistocene,central Italy). Marine and Petroleum Geology, 112: 1-11. [51] Charles V C. 1971. Depositional model,Upper Cretaceous Gallup beach shoreline,Ship Rock area,northwestern New Mexico. Journal of Sedimentary Research, 41(2): 395-409. [52] Chen J,Jiang Z X,Zhang W Y,Liu C,Han C. 2020. The study on the modern sedimentary system of Buha River Delta in Qinghai Lake. Geological Journal, 55(7): 5216-5232. [53] Chow N,George A D,Trinajstic K M,Chen Z Q,Betzler C. 2013. Stratal architecture and platform evolution of an early Frasnian syn-tectonic carbonate platform,Canning Basin,Australia. Sedimentology, 60(7): 1583-1620. [54] Davies D K,Ethridge F G,Berg R R. 1971. Recognition of barrier environments. AAPG Bulletin,55(4): 550-565. [55] Di Celma C,Pitts A,Jablonska D,Haynes, J T. 2020. Backset lamination produced by supercritical backwash flows at the beachface-shoreface transition of a storm-dominated gravelly beach(middle Pleistocene,central Italy). Marine and Petroleum Geology,112: 1-11. [56] Friedman G M,Sanders J E. 1978. Principles of Sedimentology. New York: John Wiley and Sons,488-490. [57] Gao Y,Jiang X L,Liu F,Wang X Y,Liu R H. 2017. Sedimentary characteristics and formation mechanisms of lacustrine beach-bars in the fourth member of the Shahejie Formation in the Shubei area,western depression of the Liaohe Oilfield,China. Journal of Earth Science, 28(6): 1178-1190. [58] Greenwood B,Mittler P R. 1984. Sediment Flux and Equilibrium Slopes in a Barred Nearshore-ScienceDirect. Developments in Sedimentology, 39: 79-98. [59] Grottoli E,Bertoni D,Pozzebon A,Ciavola P. 2019. Influence of particle shape on pebble transport in a mixed sand and gravel beach during low energy conditions: implications for nourishment projects. Ocean & coastal management, 169: 171-181. [60] Hall L S,Palu T J,Murray A P,Boreham C J,Edwards D S,Hill A J,Troup A. 2019. Hydrocarbon prospectivity of the Cooper Basin,Australia. AAPG Bulletin, 103: 31-63. [61] Jiang Z X,Liang S Y,Zhang Y F,Zhang S W,Qin L Z,Wei X J. 2014. Sedimentary hydrodynamic study of sand bodies in the upper subsection of the 4th Member of the Paleogene Shahejie Formation the eastern Dongying Depression,China. Petroleum Science, 11(2): 189-199. [62] Knott J R,Fantozzi J M,Ferguson K M,Keller S E,Nadimi K,Rath C A,Tarnowski J M,Vitale M L. 2012. Paleowind velocity and paleocurrents of pluvial Lake Manly,Death Valley,USA. Quaternary Research, 78: 363-372. [63] Komar P D. 1998. Beach process and sedimentation. New Jersey: Prentice Hall,1-324. [64] Konicki K M,Holman R A. 2000. The statistics and kinematics of transverse sand bars on an open coast. Marine Geology, 169(1-2): 69-101. [65] Le Mauff B,Juigner M,Ba A,Robin M,Launeau P,Fattal P. 2018. Coastal monitoring solutions of the geomorphological response of beach-dune systems using multi-temporal LiDAR datasets(Vendee coast,France). Geomorphology, 304: 121-140. [66] Lisa S H,Palu Tehani J,Murray Andrew P,Boreham Christopher J,Edwards Dianne S,Hill Anthony J,Troup Alison. 2019. Hydrocarbon prospectivity of the Cooper Basin,Australia. AAPG Bulletin, 103(1): 31-63. [67] Liu L,Chen H D,Wen H G.,Xu W L,Zhong Y J,Wang X L,Wang Z W. 2019. Facies architecture and sediment infilling processes in intrabasinal slope belts of lacustrine rift basins,Zhanhua Depression,Bohai Bay Basin. Marine and Petroleum Geology, 112: 104089. [68] Liu Q H,Zhu H T,Shu Y,Zhu X M,Yang X H,Chen L,Tan M X,Geng M Y. 2016. Provenance identification and sedimentary analysis of the beach and bar systems in the Paleogene of the Enping Sag,Pearl River Mouth Basin,South China Sea. Marine and Petroleum Geology, 70: 251-272. [69] Masselink G,Evans D,Hughes M G,Russell P. 2005. Suspended sediment transport in the swash zone of a dissipative beach. Marine Geology, 216(3): 169-189. [70] Miall A D. 1985. Architectural-element analysis: A new method of facies analysis applied to fluvial deposits. Earth Science Reviews, 22(4): 261-308. [71] Pochat S,Driessche J,Mouton V,Guillocheau F. 2005. Identification of Permian palaeowind direction from wave dominated lacustrine sediments(Lodève Basin,France). Sedimentology, 52: 809-825. [72] Potter P E. 1967. Sand bodies and sedimentary environments: a review. AAPG Bulletin, 51(3): 337-365. [73] Robin N,Billy J,Castelle B,Hesp P,Michalet R. 2020. 150 years of foredune initiation and evolution driven by human and natural processes. Geomorphology, 374(8): 1-15. [74] Rucsandra M C Kristian S,Robert B S. 2001. Detailed internal architecture of a fluvial channel sandstone determined from outcrop,cores,and 3-D ground-penetrating radar: example from the Middle Cretaceous Ferron sandstone,East-Central Utah. AAPG Bulletin, 85(9): 1583-1608. [75] Saville Thorndike. 1950. Model study of sand transport along an infinitely long,straight beach. Eos Transactions American Geophysical Union, 31(4): 555-565. [76] Schwartz R K. 2012. Bedform,texture,and longshore bar development in response to combined storm wave and current dynamics in a nearshore helical flow system. Journal of Coastal Research, 28(6): 1512-1535. [77] Shang X F,Duan T Z,Hou J G,Yan L. 2019. Spatial configuration of sand and mud in the lacustrine nearshore sand bar deposits and its geological implications. Petroleum Exploration and Development, 46(5): 954-968. [78] Shelton J W. 1967. Stratigraphic models and general criteria for recognition of alluvial,barrier-bar,and turbidity-current sand deposits. AAPG Bulletin: 51. [79] Thompson W O. 1937. Original structures of beaches,bars and dunes. Geological Society of America Bulletin, 48(6): 723-752. [80] Wang J,Cao Y C,Liu K Y,Liu,J,Kashif M. 2017. Identification of sedimentary-diagenetic facies and reservoir porosity and permeability prediction: an example from the Eocene beach-bar sandstone in the Dongying Depression,China. Marine and Petroleum Geology, 82: 69-84. [81] Wang J,Cao Y C,Xiao J,Liu K Y,Song M S. 2019. Factors controlling reservoir properties and hydrocarbon accumulation of the Eocene lacustrine beach-bar sandstones in the Dongying Depression,Bohai Bay Basin,China. Marine and Petroleum Geology, 99: 1-16. [82] Wang J H,Jiang Z X,Xian B Z,Chen J,Wang X B,Xu W M,Liu H. 2018. A method to define the palaeowind strength from lacustrine parameters. Sedimentology, 65: 461-491. [83] Wang Y,Yang S C,Zhang Y F,Lu Y,Wang Y C,Zhao Y F. 2020. Investigation of pore structure and reservoir quality of Eocene beach-bar sandstones in Dongying Depression,Bohai Bay Basin,East China. Journal of Petroleum Science and Engineering, 189: 1-15. [84] Zahid M A,Chunmei D,Lin C,Gluyas J,Jones S,Zhang X,Munawar M J. Ma C. 2016. Sequence stratigraphy,sedimentary facies and reservoir quality of Es4s,southern slope of Dongying Depression,Bohai Bay Basin,East China. Marine & Petroleum Geology, 77: 448-470. [85] Zurbuchen J,Simms A R,Warrick J A,Miller I M,Ritchie A. 2020. A model for the growth and development of wave-dominated deltas fed by small mountainous rivers: Insights from the Elwha River delta,Washington. Sedimentology, 67(5): 2310-2331.
