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天然气地球科学

• 天然气地质学 • 上一篇    下一篇

河控三角洲河口坝沉积特征及其形成过程中受水位变化的影响

张阳1，邱隆伟1，杨保良1，王军2，李际3，田美荣2，隋淑玲2   

  1. 1.中国石油大学地球科学与技术学院，山东 青岛 266580;
    2.中国石化胜利油田分公司勘探开发研究院，山东 东营 257000；
    3.中国石油新疆油田分公司实验检测研究院，新疆 克拉玛依 834000
  • 收稿日期:2015-09-15 修回日期:2015-10-23 出版日期:2016-05-10 发布日期:2016-05-10
  • 通讯作者: 邱隆伟(1967-)，男，江西南康人，教授，博士生导师，博士，主要从事矿物岩石学、沉积学及储层地质学研究. E-mail:qiulwsd@163.com.
  • 作者简介:张阳(1988-)，男，山东东营人，博士研究生，主要从事沉积学和油气地质学研究. E-mail:regogo@sina.com.
  • 基金资助:
    国家重大油气专项(编号:2011ZX05009-002);中央高校基本科研业务费专项资金项目(编号:15CX06010A)联合资助.

Research on sedimentary characteristics of river dominated delta mouth bar and influences affected by water level fluctuations during the formation

Zhang Yang1，Qiu Long-wei1，Yang Bao-liang1，Wang Jun2，Li Ji3，Tian Mei-rong2，Sui Shu-ling2   

  1. 1.School of geosciences,China University of Petroleum,Qingdao 266580,China;
    2.Research Institute of Exploration & Development,Sinopec Shengli Oilfield Company,Dongying 257000,China;
    3.Experiment Testing Institute,PetroChina Xinjiang Oilfield Company,Karamay 834000,China
  • Received:2015-09-15 Revised:2015-10-23 Online:2016-05-10 Published:2016-05-10

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摘要： 为了探讨河控三角洲河口坝在生长过程中不同发育阶段的沉积特征及其受到水位变化的影响，以鄱阳湖信江三角洲为现代沉积考察对象，通过对国内外4个典型河控三角洲高精度卫星照片的统计与分析，明确了河口坝的沉积特征及发育过程，定量计算了河口坝在不同生长阶段的参数，阐明了水位变化对河口坝生长的控制作用。研究结果表明:河口坝形成之后会继续经历一系列沉积作用，发育天然堤、决口扇、决口水道、漫流沉积、远砂坝、席状砂及泥质沉积等，形成河口坝复合体。河口坝复合体的生长可分为4个阶段:三角形河口坝复合体，V形河口坝复合体，不规则V形河口坝复合体，心滩形河口坝复合体，河口坝复合体长度与分叉前河道宽度的比值可以作为划分河口坝复合体发育阶段的重要参数。在高水位条件下，河口坝复合体的生长表现为远砂坝、前三角洲、湖相泥岩的沉积以及河水漫过天然堤发育决口扇、沼泽、支流间湾等；低水位条件下表现为河口坝的形成以及天然堤的生长。

关键词: 河控三角洲, 河口坝, 沉积特征, 形成过程, 水位变化

Abstract: In order to discuss the sedimentary characteristics and influences affected by water level fluctuations of river dominated delta mouth bar during different developmental periods,taking the Poyang lake Xinjiang delta for modern sedimentary study object,though statistics and analysis for the satellite photos of four typical river dominated deltas home or abroad,this article made clear about the development process and its sedimentary characteristics,calculated the main parameters of river mouth bar in different developmental periods,clarified the controlling effects of water level fluctuations on the development of the river mouth bar.The study results show as follows:It will experience a series of depositions after the formation of the river mouth bar and develop levee,splay,crevasse channel,sheetflood deposits,sheet sand,mud deposits,etc.The development of the river mouth bar compomer can be divided into four stages:Triangle river mouth bar compomer,V river mouth bar compomer,irregular V river mouth bar compomer,and diara-like river mouth bar compomer.The ratio of the length of river mouth bar compomer and the width of river channel before bifurcation can be used as an important parameter to divide the development stages of river mouth bar compomer.During the high water level conditions,the development of the river mouth bar compome rpresents to the deposits of far sand bar,prodelta,lake mud and the development of splay,swamp,interdistributary bay as the result of the river overflew the levee.During the low water level conditions,the development of the river mouth bar compomer presents to the development of river mouth bar and levee.

Key words: River dominated delta, River mouth bar, Sedimentary characteristics, Formation process, Water level fluctuation

中图分类号: 

  • TE121.3

[1]Jiang Zaixing.Sedimentology[M].Beijing:Petroleum Industry Press,2003.[姜在兴.沉积学[M].北京:石油工业出版社,2003.]
[2]Wen Lifeng,Wu Shenghe,Wang Yanzhong,et al.An method for anatomizing architecture of subsurface reservoir in mouth bar of fluvial dominated delta[J].Journal of Central South University:Science and Technology,2011,42(4):1072-1078.[温立峰,吴胜和,王延忠,等.河控三角洲河口坝地下储层构型精细解剖方法[J].中南大学学报:自然科学版,2011,42(4):1072-1078.]
[3]Xin Zhiguo.Architecture analyses of debouch bar of fluvial dominated delta[J].Geological Review,2008,54(4):527-531,581.[辛治国.河控三角洲河口坝构型分析[J].地质论评,2008,54(4):527-531,581.]
[4]He Wenxiang,Wu Shenghe,Tang Yijiang,et al.Detailed architecture analyses of debouch bar in Shengtuo Oilfield,Jiyang Depression[J].Petroleum Exploration and Development,2005,32(5):42-46.[何文祥,吴胜和,唐义疆,等.河口坝砂体构型精细解剖[J].石油勘探与开发,2005,32(5):42-46.]
[5]Wei Pingsheng,Wang Jiangong,Pan Shuxin,et al.Formation of the Mouth Bar and Lake Shore Bar and Their Petroleum Accumulation:An example of southern and western depositional systems in Songliao Basin[J].Xinjiang Petroleum Geology,2004,25(6):592-595.[卫平生,王建功,潘树新,等.河口坝、沿岸坝的形成及成藏机制——以松辽盆地西、南部沉积体系为例[J].新疆石油地质,2004,25(6):592-595.]
[6]Sun Yuhua,Xin Zhiguo.Remaining oil distribution and impact factors in mouth bar sands:An example from Shengtuo Field in Dongying Sag[J].Xinjiang Petroleum Geology,2009,30(2):215-218.[孙玉花,辛治国.河口坝砂体剩余油分布规律及影响因素——以东营凹陷胜坨油田为例[J].新疆石油地质,2009,30(2):215-218.]
[7]Li Qi,Hu Mingyi.Application of Seismic Sedimentology in river-delta facies and sandstone body prediction[J].Natural Gas Geoscience,2014,25(9):1341-1349.[黎祺,胡明毅.地震沉积学在河流—三角洲沉积相及有利砂体预测方面的应用[J].天然气地球科学,2014,25(9):1341-1349.]
[8]Edmonds D A,Slingerland R L.Mechanics of river mouth bar formation:Implications for the morphodynamics of delta distributary nerworks[J].Journal of Geophysical research,2007,112(F2).P.F02034.
[9]Wang Junhui,Jiang Zaixing,Zhang Yuanfu,et al.Physical simulation of deltaic deposits[J].Oil & Gas Geology,2013,34(6):758-764.[王俊辉,姜在兴,张元福,等.三角洲沉积的物理模拟[J].石油与天然气地质,2013,34(6):758-764.]
[10]Wen Zhan,Liu Zhongbao,He Youbin,et al.Sedimentation simulation experiment of braided fluvial delta of the second submember of member 3 of Paleogene Shahejie Formation in Qikou Sag of Huanghua Depression[J].Journal of Palaeogeography,2012,14(4):487-498.[文沾,刘忠保,何幼斌,等.黄骅坳陷歧口凹陷古近系沙三2亚段辫状河三角洲沉积模拟实验研究[J].古地理报,2012,14(4):487-498.]
[11]Zhu Yongjin,Yin Taiju,Shen Anjiang,et al.Experiments on shallow-lacustrine deltaic sandstone in the Ordos Basin(Upper Paleozoic),central China[J].Natural Gas Geoscience,2015,26(5):833-844.[朱永进,尹太举,沈安江,等.鄂尔多斯盆地上古生界浅水砂体沉积模拟实验研究[J].天然气地球科学,2015,26(5):833-844.]
[12]Brian R T,Gillian N T.The Table Rocks Sandstone:A fluvial,friction-dominated lobate mouth bar sandbody in the Westphalian B Coal Measures,NE England[J].Sedimentary Geology,2006,190(1-4):97-119.
[13]Wang Zhenqi,He Zhenming,Zhang Changmin,et al.Analysis on reservoir hierarchy of deltaic front outcrops:Taking Tanjiahe Outcrop in Eastern Ordos Basin for example[J].Journal of Jianghan Petroleum Institute,2004,26(3):32-36.[王振奇,何贞铭,张昌民,等.三角洲前缘露头储层层次分析——以鄂尔多斯盆地东缘潭家河剖面为例[J].江汉石油学院学报,2004,26(3):32-36.]
[14]Ma Zhenxing,Jiang Yuzhen,Wei Yuan,et al.Revision and Characters of the Poyanghu Formation(Quaternary)[J].Journal of Stratigraphy,2003,27(3):212-215.[马振兴,蒋玉珍,魏源,等.鄱阳湖组(第四系)的修订及特征[J].地层学杂志,2003,27(3):212-215.]
[15]Min Qian.On the Regularities of water level fluctuations in Poyang Lake[J].Journal of Lake Sciences,1995,7(3):281-288.[闵骞.鄱阳湖水位变化规律的研究[J].湖泊科学,1995,7(3):281-288.]
[16]Min Qian,Zhan Lasheng.Characteristics of low-water level changes in Lake Poyang during 1952-2011[J].Journal of Lake Sciences,2012,24(5):675-678.[闵骞,占腊生.1952-2011年鄱阳湖枯水变化分析[J].湖泊科学,2012,24(5):675-678.]
[17]Robert S T.Geomorphology:An approach to determining subsurface reservoir dimensions[J].AAPG Bulletin,2004,88(8):123-1147.
[18]Roberts H H.Evolution of sand-dominant subaerial phase,Atchafalaya Delta[J].AAPG Bulletin,1980,64(2):264-279.
[19]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].Journal of Palaeogeography,2014,16(2):274-284.[李燕,金振奎,李桂仔,等.江西省鄱阳湖信江决口三角洲沉积特征及模式[J].古地理学报,2014,16(2):274-284.]
[20]Jin Zhenkui,Li Yan,Gao Baishui,et al.Depositional model of modern gentle-slope delta:A case study from Ganjiang Delta in Poyang lake[J].Acta Sedimentologica Sinica,2014,32(4):710-723.[金振奎,李燕,高白水,等.现代缓坡三角洲沉积模式——以鄱阳湖赣江三角洲为例[J].沉积学报,2014,32(4):710-723.]
[21]Duan Dongping,Hou Jiagen,Liu Yuming,et al.Quantitative research of fluvial-dominated delta front sedimentary system:A case study of Poyang lake delta[J].Acta Sedimentologica Sinica,2014,32(2):270-277.[段冬平,侯加根,刘钰铭,等.河控三角洲前缘沉积体系定量研究——以鄱阳湖三角洲为例[J].沉积学报,2014,32(2):270-277.]
[22]Adam Voiland.Growing deltas in Atchafalaya bay[EB/OL].http://earthobservatory.nasa.gov/Features/WorldOfChange/wax_lake.php.
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