[1] 张景军,柳成志,曹彬彬,等. 乌尔逊凹陷南屯组湖底扇沉积特征研究[J]. 科学技术与工程,2011,11(27):6550 – 6555.Zhang Jingjun,Liu Chengzhi,Cao Binbin,et al. Thesedimentary characteristics of the lacustrine fans of NantunFormation in Wuerxun Sag,Hailaer Basin[J]. ScienceTechnology and Engineering,2011,11(27):6550 – 6555.[2] 王金铎,韩文功,于建国,等. 东营凹陷沙三段浊积岩沉积体系及其油气勘探意义[J]. 石油学报,2003,24(6):24 – 29.Wang Jinduo,Han Wengong,Yu Jianguo,et al. Turbiditysystem in the third section of Shahejie Formation ofDongying Sag andits implications on petroleum prospecting[J]. Acta Petrolei Sinica,2003,24(6):24 – 29.[3] 赵密福,信荃麟,刘泽容. 惠民凹陷临南洼陷滑塌浊积岩的分布规律及其控制因素[J]. 石油实验地质,2001,23(3):267 – 271.Zhao Mifu,Xin Quanlin,Liu Zerong. Distribution ruleand its controlling factors of slump turbidite of Linnansubsag in Huimin sag[J]. Experimental Petroleum Geology,2001,23(3):267 – 271.[4] 饶孟余,钟建华,王夕宾,等. 东营凹陷东部沙三段滑塌浊积砂体沉积特征[J]. 煤田地质与勘探,2004,32(3):15 – 17.Rao Mengyu,Zhong Jianhua,Wang Xibin,et al. Sedimentarycharacteristics of creeping turbidite sandbody ofthe Member 3 of Shahejie Formation in easetern Dongyingdepression[J]. Coal Geology & Exploration,2004,32(3):15 – 17.[5] 韦东晓,田景春,倪新锋. 湖相浊积砂体沉积特征及油气勘探意义[J]. 油气地质与采收率,2006,13(5):15 – 17.Wei Dongxiao,Tian Jingchun,Ni Xinfeng. Sedimentarycharacteristics of lacustrine turbidite sand body and its significanceon petroleum exploration[J]. Petroleum Geologyand Recovery Efficiency,2006,13(5):15 – 17.[6] 刘桠颖,徐怀民,李林,等. 准噶尔盆地阜东斜坡带深水浊积扇沉积及油气勘探意义[J]. 沉积与特提斯地质,2009,29(4):29 – 35.Liu Yaying,Xu Huaimin,Li Lin,et al. Deep-water turbiditefan deposits and their significance for the oil-gasexploration in the eastern Fukang slope zone,JunggarBasin,Xinjiang[J]. Sedimentary Geology and TethyanGeology,2009,29(4):29 – 35.[7] 张关龙,陈世悦,鄢继华,等. 三角洲前缘滑塌浊积体形成过程模拟[J]. 沉积学报,2006,24(1):50 – 55.Zhang Guanlong,Chen Shiyue,Yan Jihua,et al. Simulationof luxoturbidite in front of delta[J]. Acta SedimentologicaSinica,2006,24(1):50 – 55.[8] 鄢继华,陈世悦,姜在兴. 三角洲前缘浊积体成因及分布规律研究[J]. 石油试验地质,2008,30(1):16 – 19.Yan Jihua,Chen Shiyue,Jiang Zaixing. Genesis and distributionregularity of the turbidite bodies in the deltafront[J]. Petroleum Geology & Experiment,2008,30(1):16 – 19.[9] 韩忠义. 同沉积断层对滑塌浊积体沉积的控制作用研究以胜利油田河125 断层为例[J]. 山东科技大学学报,2008,27(3):5 – 8.Han Zhongyi. Control function of syndepositional fault onfluxoturbidite deposition:Taking Fault He125 of ShengliOilfield as an example[J]. Journal of Shandong Universityof Science and Technology,2008,27(3):5 – 8.[10] 李文龙. 同沉积断裂对沉积的控制作用以乌尔逊凹陷为例[J]. 科学技术与工程,2011,11(35):8851 – 8854.Li Wenlong. Control function of syndepositional structureon deposition[J]. Science Technology and Engineering,2011,11(35):8851 – 8854.[11] 姜在兴. 沉积学[M]. 北京:石油工业出版社,2003.[12] 马德波,李明,张佳佳,等. 鄂尔多斯盆地西南部地区延长组浊积砂体的地震识别研究[J]. 石油天然气学报,2009,31(4):73 – 78.Ma Debo,Li Ming,Zhang Jiajia,et al. Seismic identificationof turbidite sandbody in Yanchang Formation in thesouth of Ordos Basin[J]. Journal of Oil and Gas Technology,2009,31(4):73 – 78.[13] 操应长,刘晖. 湖盆三角洲沉积坡度带特征及其与滑塌浊积岩分布关系的初步探讨[J]. 地质论评,2007,53(4):454 – 458.Cao Yingchang,Liu Hui. Discussion on the relationshipbetween distribution of fluxoturbidite and depositional slopeof delta in Lacustrine Basin[J]. Geological Review,2007,53(4):454 – 458.