Sedimentary model and controlling factors of modern beach-bar sediments in east coast of Xiashan Lake in Shandong Province
Bai Li-Ke1, Qiu Long-Wei1,2,3, Yang Yong-Qiang1,2,3, Du Shuang-Hu1, Yang Bao-Liang1, Han Xiao-Tong1
1 School of Geosciences,China University of Petroleum(East China),Shandong Qingdao 266580,China; 2 Key Laboratory of Deep Oil and Gas,Shandong Qingdao 266580,China; 3 Laboratory for Marine Mineral Resources,Qingdao National Laboratory for Marine Science and Technology,Shandong Qingdao 266237,China
Abstract:Beach-bars, one of the important hydrocarbon reservoirs formed in the coastal zone,become the exploration target in terms of subtle reservoirs. In order to figure out the sedimentary model of beach bars deposited in the east coast of Xiashan Lake,a detailed study on sedimentary characteristics and controlling factors of beach-bars was carried out by using ground penetrating radar (GPR) and grain size analysis. The results show that,the east coast of Xiashan Lake has developed two types of sedimentary systems including beach bars and eolian dunes. The eolian sediments in the early stage are well-sorted fine-grained sandstones, which are characterized by large tabular cross-bedding and two-segment pattern on grain size cumulative frequency plot. The beach bars sediments are reverse graded medium-grained sandstone and feature the low-continuity tabular cross-bedding. Plant roots,scouring structure,interbedding of sand and mud and three-segment pattern on on grain size cumulative frequency plot arethe typical characteristics of beach ̄bar deposits. The saltation proportion is divided into two different parts indicating high energy hydrodynamic condition. Layered reflecting structures can be confirmed through GPR which implies the eolian sediments depositional pattern. The analyses of environmentally sensitive components of the grain size of eolian sediments suggest two different hydrodynamic environment. In conclusion,eolian sediments and the change of paleogeomorphy environment depend on wind action. The coastal erosion plays an important role in the early stage of the position and sand supply for beach bars. According to the sedimentary model as well as its formation mechanism,we propose a ‘wind transporting-wave modifying’ sedimentary system,which will be helpful for identification of beach bars and the prediction of favorable reservoir.
Bai Li-Ke,Qiu Long-Wei,Yang Yong-Qiang et al. Sedimentary model and controlling factors of modern beach-bar sediments in east coast of Xiashan Lake in Shandong Province[J]. JOPC, 2020, 22(2): 278-294.
[1] 白旸,王乃昂,何瑞霞,李景满,赖忠平. 2011. 巴丹吉林沙漠湖相沉积的探地雷达图像及光释光年代学证据. 中国沙漠, 31(4): 842-847. [Bai Y,Wang N A,He R X,Li J M,Lai Z P.2011. Ground penetrating radar images and optically stimulated luminescence dating for lacustrine deposition of the Badain Jaran Desert. Journal of Desert Research, 31(4): 842-847] [2] 操应长,王健,刘惠民,贾光华,万念明. 2009. 东营凹陷南坡沙四上亚段滩坝砂体的沉积特征及模式. 中国石油大学学报(自然科学版), 33(6): 5-10. [Cao Y C,Wang J,Liu H M,Jia G H,Wan N M.2009. Sedimentary characteristics and models of beach-bar sandbodies in the upper part of the Fourth Member of Paleogene in the south slope of Dongying depression. Journal of China University of Petroleum(Edition of Natural Science), 33(6): 5-10] [3] 操应长,王健,刘惠民. 2010. 利用环境敏感粒度组分分析滩坝砂体水动力学机制的初步探讨: 以东营凹陷西部沙四上滩坝砂体沉积为例. 沉积学报, 28(2): 274-284. [Cao Y C,Wang J,Liu H M.2010. Preliminary study on the hydrodynamic mechanism of beach-bar sandbodies with environmentally sensitive grain size components: A case study from beach-bar sandbody sediments of the upper part of the Fourth Member of the Shahejie Formation in the western Dongying depression. Acta Sedimentologica Sinica, 28(2): 274-284] [4] 陈骥,姜在兴,张万益,刘超,许文茂. 2018. “源-汇”沉积体系主导下的现代风成相发育模式探讨: 以青海湖东岸为例. 中国沙漠, 38(5): 103-112. [Chen J,Jiang Z X,Zhang W Y,Liu C,Xu W M.2018. Discussion on depositional models of modern aeolianfacies under the guidance of source-to-sink system theory: A case study of east coast of Qinghai Lake. Journal of Desert Research, 38(5): 103-112] [5] 陈桥,刘东艳,陈颖军,申旭红,蒋金杰,李欣,姜晓华. 2013. 粒级—标准偏差法和主成分因子分析法在粒度敏感因子提取中的对比. 地球与环境, 41(3): 319-325. [Chen Q,Liu D Y,Chen Y J,Shen X H,Jiang J J,L X,Jiang X H.2013. Comparative analysis of grade-standard deviation method and factors analysis method for environmental sensitive factor analysis. Earth and Environment, 41(3): 319-325] [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, 28(3): 1-4. [Chen S Y,Yang J P,Cao Y C.2000. Sedimentary characteristics of two kinds of beach-bars of Oligocene Shahejie Formation in western Huimin depression,China. Coal Geology & Exploration, 28(3): 1-4] [7] 德勒恰提,王威,王利,阿迪力江. 2012. 粒度分析在吉木萨尔凹陷梧桐沟组沉积相研究中的应用. 新疆大学学报(自然科学版), 29(2): 142-149. [Deleqiati,Wang W,Wang L,W L,Adilijiang.2012. Application of particle size characteristics analysis in sedimentary facies research of the Permi-an Wutonggou Formation in the Jimusaer depression. Journal of Xinjiang University: Natural Science Edition, 29(2): 142-149] [8] 邓世彪,关平,张鹏飞. 2017. 东营凹陷青南地区沙四上亚段物源沉积体系与滩坝分布. 沉积学报, 35(3): 561-576. [Deng S B,Guan P,Zhang P F.2017. Provenance,sedimentary system and beach bar distribution of the Upper Es4 in Qingnan area,Dongying Depression. Acta Sedimentologica Sinica, 35(3): 561-576] [9] 董玉祥. 2002. 海岸现代风成砂粒度参数特征的研究: 以中国温带海岸为例. 沉积学报, 20(4): 656-662. [Dong Y X.2002. Characteristics of grain size parameters of modern coastal Aeolian sands in themperate coastal region in China. Acta Sedimentologica Sinica, 20(4): 656-662] [10] 董玉祥. 2003. 国内外海岸风成砂粒度参数特征的比较与分析. 中山大学学报(自然科学版), 42(4): 110-113. [Dong Y X.2003. The comparison and analysis of grain size parameters of coastal Aeolian sands in China and abroad. Acta Scientiarum Naturalium Universitatis Sunyatseni, 42(4): 110-113] [11] 董玉祥. 2006. 中国海岸风沙地貌的类型及其分布规律. 海洋地质与第四纪地质, 26(4): 99-104. [Dong Y X.2006. The coastal Aeolian geomorphic types and their distribution pattern in China. Marine Geology & Quaternary Geology, 26(4): 99-104] [12] 高晓梅,马守强,董晨娥,张芹,袁静. 2009. 近45年潍坊市降水气候特征及水资源现状分析. 中国农业气象,30(S1): 16-21. [Gao X M,Ma S Q,Dong C E,Zhang Q,Yuan J.2009. Analysis on precipitation and water resource in Weifang city in Last 45 years. Chinese Journal of Agrometeorology,30(S1): 16-21] [13] 郭照河,杨化勇,李飞,毕钦祥,史光亭. 2004. 峡山水库富营养化评价与对策研究. 水文, 24(4): 50-52. [Guo Z H,Yang H Y,Li F,Bi Q X,Shi G T.2004. Eutrophication assessment for the Xiashan reservoir and countermeasures rearch. Hydrology, 24(4): 50-52] [14] 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] [15] 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] [16] 姜在兴,王雯雯,王俊辉,李庆,张元福. 2017. 风动力场对沉积体系的作用. 沉积学报, 35(5): 863-876. [Jiang Z X,Wang W W,Wang J H,Li Q,Zhang Y F.2017. The influence of wind field on depositional systems,Acta Sedimentologica Sinica, 35(5): 863-876] [17] 赖海成,李志忠,靳建辉,邓涛,姜锋,于晓莉,苑秀全,申健玲,龚松柏. 2016. 基于GPR图像的福建海坛岛北部海岸冲积扇沉积构造及其成因的初步研究. 沉积学报, 34(4): 645-652. [Lai H C,Li Z Z,Jin J H,Deng T,Jiang F,Yu X L,Yuan X Q,Shen J L,Gong S B.2016. Unravelling the sedimentary structure of coastal alluvial fan and its origin in the Northern Haitan Island,Fujian,using ground penetrating radar. Acta Sedimentologica Sinica, 34(4): 645-652] [18] 赖海成,李志忠,靳建辉,邓涛,姜锋,苑秀全,申健玲,于晓莉,徐晓琳,程延. 2017. 福建海坛岛北部海岸带冲积扇沉积构造及其发育模式. 地质学报, 91(8): 1878-1893. [Lai H C,Li Z Z,Jin J H,Deng T,Jiang F,Yuan X Q,Shen J L,Yu X L,Xu X L,Cheng Y.2017. Sedimentary structure and developing model of coastal alluvial fan along the Northern Coast of Haitan Island,Fujian. ActaGeologicaSinica, 91(8): 1878-1893] [19] 李国斌,姜在兴,陈诗望,冯磊,张善文,隋风贵,刘惠民. 2008. 利津洼陷沙四上亚段滩坝沉积特征及控制因素分析. 中国地质, 35(5): 911-921. [Li G B,Jiang Z X,Chen S W,Feng L,Zhang S W,Sui F G,Liu H M.2008. Sedimentary characteristics and controlling factors of beach bars in the Upper Submember of the Fouth Member of the Shahejie Formation in the Lijin subasin. Geology in China, 35(5): 911-921] [20] 李腾飞,李金凤,鲁瑞洁,刘小槺,陈璐. 2017. 青海湖东岸沙地风成沉积物粒度敏感组分及其古气候意义. 中国沙漠, 37(5): 878-884. [Li T F,Li J F,Lu R J,Liu X K,Chen L.2017. Extraction of grain-size components with environmentally sensitivity of Aeolian sediments in Eastern Shore of Qinghai lake and their palaeoclimatic implications. Journal of Desert Research, 37(5): 878-884] [21] 刘澜波,钱荣毅. 2015. 探地雷达: 浅表地球物理科学技术中的重要工具. 地球物理学报, 58(8): 2606-2617. [Liu L B,Qian R Y.2015. Ground penetrating radar: A critical tool in near-surface geophysics. Chinese Journal of Geophysics, 58(8): 2606-2617] [22] 刘立安,姜在兴. 2011. 四川盆地古近纪沙漠沉积特征及古风向意义. 地质科技情报, 30(2): 63-68. [Liu L A,Jiang Z X.2011. Depositional features of the desert in the Paleogene Sichuan Basin and the significance for the reconstruction of palaeowind direction. Geological Science and Technology Information, 30(2): 63-68] [23] 李志德,程守田,蒋磊,李娟,郭秀蓉. 2004. 风成沙丘间沉积成因类型与风成垂向层序: 以鄂尔多斯早白垩世内陆古沙漠为例. 地质科技情报, 23(3): 30-34. [Li Z D,Cheng S T,Jiang L,Li J,Guo X R.2004. Interdune sedimentary genetic types and Aeolian vertical sequence: An example from Early Cretaceous continental paleodesert of Ordos. Geological Science and Technology Information, 23(3): 30-34] [24] 隆浩,王乃昂,马海州,李育. 2007. 腾格里沙漠西北缘湖泊沉积记录的区域风沙特征. 沉积学报, 25(4): 626-631. [Long H,Wang N A,Ma H Z,Li Y.2007. Eolian activity and environment evolution history recorded by the Qingtu Lake,NW Tengger Desert. Acta Sedimentologica Sinica, 25(4): 626-631] [25] 路慎强,王健,操应长,谭明友,张营革. 2013. 车西洼陷沙二段滩坝砂体粒度特征及其水动力学意义. 油气地质与采收率, 20(3): 26-29. [Lu S Q,Wang J,Cao Y C,Tan M Y,Zhang Y G.2013. Study on characteristics and hydro-dynamic significance of grain size components of beachbar sand-bodies,second member of Shahejie Formation,Chexi Sag. Petroleum Geology and Recovery Efficiency, 20(3): 26-29] [26] 梅冥相,于炳松,靳卫广. 2004. 塔里木盆地北缘库车盆地白垩系风成砂岩研究: 以库车河剖面为例. 地质通报, 23(12): 1221-1227. [Mei M X,Yu B S,Jin W G.2004. Cretaceous eolian sandstones in the Kuqa basin on the northern margin of the Tarim basin: A case study of the Kuqa River section. Geological Bulletin of China, 23(12): 1221-1227] [27] 梅冥相,苏德辰. 2014. 甘肃张掖地区白垩系风成砂岩沉积序列: 祁连山白垩纪隆升的沉积学响应. 古地理学报, 16(2): 143-156. [Mei M X,Su D C.2014. Cretaceous sedimentary succession of eolian sandstones in Zhangye Region of Gansu Province: Sedimentological response to the Cretaceous uplift of Qilian Mountains. Journal of Palaeogeography(Chinese Edition), 16(2): 143-156] [28] 牛光明,强明瑞,宋磊,郎丽丽,王立强. 2010. 5000 a来柴达木盆地东南缘风成沉积记录的冬季风演化. 中国沙漠, 30(5): 1031-1039. [Niu G M,Qiang M R,Song L,Lang L L,Wang L Q.2010. Change of Eastern Asian winter monsoon recorded by Aeolian deposits over the past 5000 years at the Southeastern Margin of Qaidam Basin. Journal of Desert Research, 30(5): 1031-1039] [29] 邱隆伟,周军良,姜在兴,王新征. 2009. 峡山湖沙坝的现代沉积. 海洋地质与第四纪地质, 29(4): 135-141. [Qiu L W,Zhou J L,Jiang Z X,Wang X Z.2009. A recent sedimentary study on sand bar in Xiashan Lake. Marine Geology & Quaternary Geology, 29(4): 135-141] [30] 邱隆伟,周军良,王新征,蔡宏兴,张振哲. 2010. 山东峡山湖滩砂的现代沉积特征研究. 矿物岩石地球化学通报, 29(2): 142-148. [Qiu L W,Zhou J L,Wang X Z,Cai H X,Zhang Z Z.2010. A characteristics study of neoteric sediment to the beach of Xiashan Lake in Shandong Province. Bulletin of Mineralogy,Petrology and Geochemistry, 29(2): 142-148] [31] 商晓飞,侯加根,程远忠,安振月,姚瑞香,李燕. 2014. 厚层湖泊滩坝砂体成因机制探讨及地质意义: 以黄骅坳陷板桥凹陷沙河街组二段为例. 地质学报, 88(9): 1705-1718. [Shang X F,Hou J G,Cheng Y Z,An Y Z,Yao R X,Li Y.2014. Formation mechanism of the thick layer lacustrine beach-bar and its geological implications: An example of the 2nd Member of the Shahejie Formation in Banqiao Sag. Acta Geologica Sinica, 88(9): 1705-1718] [32] 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 Xiashan lake. Acta Sedimentologica Sinica, 36(5): 877-889] [33] 沈星,褚忠信,王玥铭,李应坤,苗安洋,梁玉蕾. 2015. 北黄海西部与南黄海中部泥质区岩心敏感粒级及其环境意义. 沉积学报, 33(1): 124-133. [S X,Chu Z X,Wang Y M,Li Y K,Miao A Y,Liang Y L.2015. Sensitive grain size and its environmental significance of modern mud patches in Southern and Northern Parts of the Yellow Sea. Acta Sedimentologica Sinica, 33(1): 124-133] [34] 时瑞坤,高秋菊,韩小锋,巴素玉,师涛,韩敏. 2018. 车镇凹陷沙二段滩坝砂体沉积特征及控制因素. 岩性油气藏, 30(2): 50-57. [Shi R K,Gao Q J,Han X F,Ba S Y,Shi T,Han M.2018. Sedimentary characteristics and controlling factors of beach-bar sandbodies of the second member of Shahejie Formation in Chezhen Sag. Lithologic Reservoirs, 30(2): 50-57] [35] 孙有斌,高抒,李军. 2003. 边缘海陆源物质中环境敏感粒度组分的初步分析. 科学通报, 48(1): 83-86. [Sun Y B,Gao S,Li J.2003. Preliminary analysis of grain-size populations with environmentally sensitive terrigenous components in marginal sea setting. Chinese Science Bulletin, 48(1): 83-86] [36] 唐丽,董玉祥. 2015. 华南海岸现代风成沙与海滩沙的粒度特征差异. 中国沙漠, 35(1): 14-23. [Tang L,Dong Y X.2015. Characteristics of grain size of modern Aeolian sand and beach sand in coast of South China. Journal of Desert Research, 35(1): 14-23] [37] 滕珊,冯秀丽,田动会,姜波,王晓明,姜建新. 2018. 山东半岛泥质区沉积物敏感粒级分析及其环境意义. 中国海洋大学学报(自然科学版),48(S1): 71-81. [Teng S,Feng X L,Tian D H,Jiang B,Wang X M,Jiang J X.2018. Sensitive grain size components and their environmental significance of sediment in the Shandong Peninsula. Periodical of Ocean University of China,48(S1): 71-81] [38] 田继军,姜在兴. 2012. 惠民凹陷与东营凹陷沙四上亚段滩坝沉积特征对比与分析. 吉林大学学报(地球科学版), 42(3): 612-623. [Tian J J,Jiang Z X.2012. Comparison and analysis of beach bars sedimentary characteristics of upper Es4 in Huimin and Dongying Depression. Journal of Jilin University(Earth Science Edition), 42(3): 612-623] [39] 王杰. 2018. 无人机航摄技术在峡山水库测量中的应用. 测绘通报,(8): 150-152. [Wang J.2018. The application of UAV aerial photography in measurement of Xiashan Reservoir. Bulletin of Surveying and Mapping, (8): 150-152] [40] 王升兰,姜在兴,邱隆伟,刘晖. 2014. 现代滩砂沉积特征及其对油气勘探的启示. 油气地质与采收率, 21(1): 16-19. [Wang S L,Jiang Z X,Qiu L W,Liu H.2014. Characteristics of the modern beach and their significance to hydrocar-bon exploration. Petroleum Geology and Recovery Efficiency, 21(1): 16-19] [41] 王旭影,姜在兴. 2018. 苏北盆地海安凹陷古近系阜三段滩坝沉积特征. 油气地质与采收率, 25(5): 57-64. [Wang X Y,Jiang Z X.2018. Sedimentary characteristics of beach-bar in the 3rd member of Paleogene Funing Formation in Hai’an Sag,North Jiangsu Basin. Petroleum Geology and Recovery Efficiency, 25(5): 57-64] [42] 温小浩,李保生,孟洁,杨庆江,郑琰明,牛东风,王丰年,蔡瑜杭. 2015.150-20ka BP福建东部平潭岛海岸风成沉积的粒度特征及其环境意义. 中国沙漠, 35(6): 1473-1482. [Wen X H,Li B S,Meng J,Yang Q J,Zheng Y M,Niu D F,Wang F N,Cai Y H.2015. Grain size characteristics of coastal Aeolian sediments in the Pingtan Island of Fujian,China,and their implications for the paleoenvironment from 150 ka BP to 20ka BP. Journal of Desert Research, 35(6): 1473-1482] [43] 向荣,杨作升,Saito Y,郭志刚,范德江,李云海,肖尚斌,石学法,陈木宏. 2006. 济州岛西南泥质区近2300 a来环境敏感粒度组分记录的东亚冬季风变化. 中国科学(D辑: 地球科学), 36(7): 654-662. [Xiang R,Yang Z S,Saito Y,Guo Z G,Fang D J,Li Y H,Xiao S B,Shi X F,Chen M H.2006. East Asia Winter Monsoon changes inferred from environmentally sensitive grain-size component records during the last 2300 years in mud area southwest off Cheju Island,ECS. Science in China Series D: Earth Sciences, 36(7): 654-662] [44] 徐树建. 2007. 风成沉积物环境敏感粒度指标的提取及意义. 干旱区资源与环境, 21(3): 95-98. [Xu S J.2007. Analysis of grain-size populations with environmentally sensitive components in Aeolian deposits and their implications. Journal of Arid Land Resources and Environment, 21(3): 95-98] [45] 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] [46] 姚正毅,李晓英,肖建华. 2015. 青海湖滨土地沙漠化驱动机制. 中国沙漠, 35(6): 1429-1437. [Yao Z Y,Li X Y,Xiao J H.2015. Driving mechanism of sand desertification around the Qinghai Lake. Journal of Desert Research, 35(6): 1429-1437] [47] 张秀珍,张文煜,宋嘉尧,白庆梅. 2008. 潍坊市近45年气候特征分析. 山东气象, 28(1): 14-17. [Zhang X Z,Zhang W Y,Song J Y,Bai Q M.2008. Analysis of climate characteristics of Weifang city in recent 45 years. Journal of Shandong Meteorology, 28(1): 14-17] [48] 张宇. 2008. 东营凹陷西部沙四段上亚段滩坝砂体的沉积特征. 油气地质与采收率, 15(6): 35-38. [Zhang Y.2008. Sedimentary characteristics of beach-bar sandbodies in Es4 member in the western Dongying Depression. Petroleum Geology and Recovery Efficiency, 15(6): 35-38] [49] 赵西西,王天阳,朱丽东,叶玮,李凤全,谷喜吉. 2015. 庐山JL剖面粒度敏感组分的提取与环境意义初探. 地理与地理信息科学, 31(2): 115-118. [Zhao X X,Wang T Y,Zhu L D,Ye W,Li F Q,Gu X J.2015. Extraction of environmentally sensitive grain size group from JL Section and initial exploration of its environmental significance. Geography and Geo-Information Science, 31(2): 115-118] [50] 郑岩,胡志强. 2016. 水库渔业资源逆民营化管理方式研究: 以山东省峡山水库为例. 中国高新技术企业,(23): 7-10. [Zheng Y,Hu Z Q.2016. Research on the management method of reversed privatization of reservoir fishery resources. China High-Tech Enterprises,(23): 7-10] [51] 朱如凯,白斌,袁选俊,罗忠,汪沛,高志勇,苏玲,李婷婷. 2013. 利用数字露头模型技术对曲流河三角洲沉积储层特征的研究. 沉积学报, 31(5): 867-877. [Zhu R K,Bai B,Yuan X J,Luo Z,Wang P,Gao Z Y,Su L,Li T T.2013. A new approach for outcrop characterization and geostatistical analysis of meandering channels sandbodies within a delta plain setting using digital outcrop models: Upper Triassic Yanchang tight sandstone formation,Yanhe outcrop,Ordos Basin. Acta Sedimentologica Sinica, 31(5): 867-877] [52] 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. Sedimentary characteristics and models of the beach-bar reservoirs in faulted down lacustrine basins. Acta Sedimentologica Sinica, 12(2): 20-28] [53] Bristow C,Mountney N P.2013. Aeolian Stratigraphy. Treatise on Geomorphology.San Diego: Academic Press,246-268. [54] Chu Z X,Sun X G,Zhai S K,Xu K H.2006. Changing pattern of accretion/erosion of the modern Yellow River(Huanghe)subaerial delta,China: Based on remote sensing images. Marine Geology, 227(1): 13-30. [55] Prins M A,Postma G,Weltje G J.2000. Controls on terrigenous sediment supply to the Arabian Sea during the late Quaternary: The Makran continental slope. Marine Geology, 169(3): 351-371. [56] Pye K,Tsoar H.1987. The mechanics and geological implications of dust transport and deposition in deserts with particular reference to loess formation and dune sand diagenesis in the northern Negev,Israel. Geological Society London Special Publications, 35(1): 139-156. [57] Sun D H,Bloemendal J,Rea D K,Wagonerdenberghe J,Jiang F C,An Z S,Su R X.2002. Grain-size distribution function of polymodal sediments in hydraulic and aeolian environments,and numerical partitioning of the sedimentary components. Sedimentary Geology, 152(3): 263-277. [58] Vriend N M,Hunt M L,Clayton R W.2012. Sedimentary structure of large sand dunes: Examples from Dumont and Eureka dunes,California. Geophysical Journal International, 190(2): 981-992.