Depositional characteristics and model for crevasse delta of Xinjiang River in Poyang Lake area, Jiangxi Province
Li Yan1,2, Jin Zhenkui1,2, Li Guizi1,2, Gao Baishui1,2, Shi Liang1,2
1 College of Geosciences,China University of Petroleum(Beijing),Beijing 102249; 2 State Key Laboratory of Petroleum Resource and Prospecting,China University of Petroleum(Beijing),Beijing 102249
Abstract:Based on field investigation,shallow boreholes,exploration trench and google earth,the crevasse delta of Xinjiang River in Poyang Lake area,Jiangxi Province is studied in detail. The crevasse delta is formed when flood breaches the natural levee on west bank of the Xinjiang River and flows into the flood lake nearby. The delta is bird-foot shape in the plane,and is distributed overall perpendicular to the main channel trend of the Xinjiang River. In the transverse profile,the depositional body of the crevasse delta is lenticular in the lateral,and overlies the previous deposits of wetlands or flood lake. The crevasse delta can be divided into three subfacies,i.e. crevasse delta plain,crevasse delta front and crevasse prodelta. On the delta plain,there are crevasse channels,natural levees,abandoned crevasse channels,and wetlands. Crevasse channels can be further divided into waterways,point bars and branch mouth bars. On the delta front,mouth bars and inter-distributary bays are developed. Sheet sand is not developed,because the flood lake is small in scale and wave energy is not high enough to create longshore current to modify mouth bar and crevasse channel sand bodies. The depositional characteristics of the crevasse delta are controlled jointly by fluvial and flood lake process. The evolution model of the crevasse delta can be divided into four stages:Main channel natural levee growth stage,early crevasse stage,prorogation and channel branching stage,channel branching and abandoning stage.
Li Yan,Jin Zhenkui,Li Guizi et al. Depositional characteristics and model for crevasse delta of Xinjiang River in Poyang Lake area, Jiangxi Province[J]. JOPC, 2014, 16(2): 274-284.
陈廷笔,徐立平. 2005. 信江流域洪涝干旱灾害成因分析及防御对策[J]. 江西水利科技,31(2):67-70. 葛道凯,杨起,付泽明,等. 1990. 陕西榆林地区延安组湖滨下三角洲平原沉积中的决口扇三角洲沉积及其意义[J]. 现代地质,4(3):51-59. 金振奎,何苗. 2011. 三角洲沉积模式的新认识[J]. 新疆石油地质,32(5):443-446. 金振奎,苏奎,张永生,等. 2011. 湿地的沉积特征及石油地质意义[J]. 中国石油大学学报(自然科学版), 35(3):1-6. 李少华,卢文涛. 2011. 基于沉积过程的储集层随机建模方法: 以河流相储集层为例[J]. 古地理学报,13(3):325-333. 鹿洪友,袁静,陈小宏,等. 2008. 渤海湾盆地垦东凸起北坡新近系馆陶组上段沉积相模式探讨[J]. 古地理学报,10(5):511-520. 杨玉卿,田洪,孟杰,等. 2001. 渤海湾中部南堡35-2地区新第三系河流沉积及油气勘探意义[J]. 古地理学报,3(4):77-84. 詹云军,薛重生. 2002. 长江荆江河段古决口扇遥感专题分析及成因研究[J]. 地质科技情报,21(4):55-59. 朱海虹,郑长苏,王云飞,等. 1981. 鄱阳湖现代三角洲沉积相研究[J]. 石油与天然气地质,2(2):89-103. Bernal C,Christophoul F,Darrozes J, et al. 2013. Crevassing and capture by floodplain drains as a cause of partial avulsion and anastmosis(lower Rio Pastaza,Peru)[J]. Journal of South American Earth Science,44:63-74. Davies-Vollum K S,Kraus M J. 2001. A relationship between alluvial backswamps and avulsion cycles:An example from the Willwood Formation of the Bighorn Basin,Wyoming[J]. Sedimentary Geology,140:235-249. Elliott T. 1974. Interdistributary bay sequences and their genesis[J]. Sedimentology,21:611-622. Farrell K M. 2001. Geomorphology,facies architecture,and high-resolution,non-marine sequence stratigraphy in avulsion deposits,Cumberland Marshes,Saskatchwan[J]. Sedimentary Geology,139:93-150. Fielding C R. 1984. Upper delta plain lacustrine and fluviolacustrine facies from the Westphalian of the Durham coalfield,NE England[J]. Sedimentology,31:547-567. Hajek E A,Wolonsky M A. 2012. Simplified process modeling of river avulsion and alluvial architecture: Connecting models and field data[J]. Sedimentary Geology,257-260:1-30. Jin Zhenkui, Gu Junfeng, Su Nina, et al. 2009. Depositinal characteristics and petroleum geological significance of wetland [J]. Petroleum Science, 6(4):347-353. Jones H L,Hajek E A. 2007. Characterizing avulsion stratigraphy in ancient alluvial deposits[J]. Sedimentary Geology,202:124-137. Perez-arlucea M,Smith N D. 1999. Depositional patterns following the 1870s avulsion of the Saskatchewan river(Cumberland and marshes,Saskatchewan,Canada)[J]. Journal of Sedimentary Research,69(1):62-73. Smith N D,Perez-aelucea M. 1994. Fine grained splay deposition in the avulsion belt of the lower Saskatchewan river,Canada[J]. Journal of Sedimentary Research,64(2):159-168. Stouthamer E. 2001. Sedimentary products of avulsions in the Holocene Rhine-Meuse Delta,the Netherlands[J]. Sedimentary Geology,145:73-92.