二连盆地白音查干凹陷下白垩统腾格尔组滑塌-浊流沉积特征——以达49井为例

doi:10.7623/syxb201707005

石油学报 ›› 2017, Vol. 38 ›› Issue (7): 777-792.DOI: 10.7623/syxb201707005

二连盆地白音查干凹陷下白垩统腾格尔组滑塌-浊流沉积特征——以达49井为例

高红灿¹, 郑荣才², 肖斌³, 刘云³, 郑玲³, 栾艳春³, 刘虹利¹

1. 重庆科技学院石油与天然气工程学院重庆 401331;
2. 成都理工大学油气藏地质及开发工程国家重点实验室四川成都 610059;
3. 中国石油化工股份有限公司中原油田分公司物探研究院河南濮阳 457001

收稿日期:2016-12-26 修回日期:2017-03-19 出版日期:2017-07-25 发布日期:2017-08-10
通讯作者: 高红灿,男,1969年11月生,1995年获成都理工学院地质学专业学士学位,2007年获成都理工大学沉积学专业博士学位,现为重庆科技学院石油与天然气工程学院副教授,主要从事沉积学和石油地质学的教学与研究工作。Email:gaohongcan@126.com
作者简介:高红灿,男,1969年11月生,1995年获成都理工学院地质学专业学士学位,2007年获成都理工大学沉积学专业博士学位,现为重庆科技学院石油与天然气工程学院副教授,主要从事沉积学和石油地质学的教学与研究工作。Email:gaohongcan@126.com
基金资助:
重庆市科委前沿与应用基础研究（一般）项目（cstc2014jcyjA90022）和重庆科技学院科研基金项目（CK2016B14）资助。

Slump-turbidite sedimentary characteristics of the Lower Cretaceous Tenggeer Formation in Baiyinchagan sag of Erlian Basin:a case study of Well Da 49

Gao Hongcan¹, Zheng Rongcai², Xiao Bin³, Liu Yun³, Zheng Ling³, Luan Yanchun³, Liu Hongli¹

1. School of Petroleum Engineering, Chongqing University of Science & Technology, Chongqing 401331, China;
2. State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation, Chengdu University of Technology, Sichuan Chengdu 610059, China;
3. Geophysical Research Institute, Sinopec Zhongyuan Oilfield Company, Henan Puyang 457001, China

Received:2016-12-26 Revised:2017-03-19 Online:2017-07-25 Published:2017-08-10

摘要/Abstract

摘要：

为厘清白音查干凹陷达49井附近下白垩统腾格尔组下段发育的地层厚度异常体的空间形态、形成机制、形成条件、物质来源等，以利于白音查干凹陷的地层-岩性油气藏勘探，综合运用地层对比、地震反射、钻井岩心和测井数据等资料，主要对其空间发育、沉积构造、结构组分和测井曲线等沉积特征进行了较深入的研究。结果表明该地层厚度异常体主要是由其中的薄层粉-细砂岩叠加造成，在空间上呈透镜状，并与达尔其辫状河三角洲前缘相连接；滑塌砂体中大量发育包卷变形层理及呈拉长状和撕裂状等不规则塑性变形泥砾，其砂体底部冲刷面发育；浊积砂体中大量发育正粒序层理及液化砂岩脉构造，其砂体底部槽模和重荷模较发育。进一步推测白音查干凹陷达49井附近下白垩统腾格尔组下段发育的地层厚度异常体主要为达尔其辫状河三角洲前缘砂体在地震作用触发下发生滑塌，并随着滑塌块体在重力搬运过程中水体的不断加入而逐步转变为浊流沉积；滑塌-浊流沉积形成的前提条件为地形坡度大和具一定的外界触发机制，必要条件为深水滞水环境（形成于湖侵期）和充沛的物源。该滑塌-浊流不发育固定的补给水道，运移距离短，所形成的浊积体规模小、厚度薄，且呈较孤立的透镜状和舌状等，但其数量多、分布广，且靠近烃源岩，只要其具一定的累计厚度，则易于形成岩性油气藏的有利富集带。

关键词: 二连盆地, 白音查干凹陷, 下白垩统, 腾格尔组, 滑塌沉积, 浊流沉积

Abstract:

In this study, comprehensively using the stratigraphic correlation, seismic reflection, core and logging curves data, a deep study was conducted mainly on the sedimentary characteristics, including spatial development, sedimentary tectonics, structural components and logging data of the anomalous body. This aims to clarify the spatial morphology, formation mechanism, formation conditions and material source of the strata thickness anomalous body developed in the lower Member of the Lower Cretaceous Tenggeer Formation near the Well Da 49 within Baiyinchagan sag, and then make contribution to the exploration of stratigraphic-lithologic oil-gas reservoir of Baiyinchagan sag. The results indicate that the strata-thickness anomalous body was mainly formed by the superimposition of thin-layer siltstone and fine-grained sandstone therein, and it is lenticular and connecting with the Daerqi braided river delta front; plenty of rolled convolute bedding as well as elongated, lacerated and irregular plastic deformed boulder clay are well developed in slumping sand body, and erosional surface is developed at its bottom; plenty of normal graded bedding and liquefied sandstone dikes are well developed in turbidite sand body, while flute cast and load cast are well developed at its bottom. Further, it is speculated that the sand body in the Daerqi braided river delta front was slumped due to the trigger of seismism, and the slump block was gradually transformed into turbidite flow under the continuous addition of water during the process of gravity transportation, and then deposited, thus forming the strata-thickness anomalous body developed in the lower member of the Lower Cretaceous Tenggeer Formation near the Well Da 49 within Baiyinchagan sag; the preconditions for the formation of slump-turbidites sedimentation are the large topographic slope and a certain external triggering mechanism, and its necessary conditions are the deep-water stagnant environment (forming in the lacustrine transgression period) and abundant material sources. The slump-turbidites had no fixed feeder channel, and the transport distance of the flow was short; therefore, the formed turbidites are characterized by small size and thin thickness, relatively isolatedly distributed in the shape of lenses and tongue, large in quantity, and widespread near the hydrocarbon source rock. Thus, as long as the turbidites have a certain accumulative thickness, the enrichment zone of lithologic oil-gas reservoirs can be easily formed in the study area.

Key words: Erlian Basin, Baiyinchagan sag, Lower Cretaceous, Tenggeer Formation, slump deposits, turbidity deposits

中图分类号:

TE122

高红灿, 郑荣才, 肖斌, 刘云, 郑玲, 栾艳春, 刘虹利. 二连盆地白音查干凹陷下白垩统腾格尔组滑塌-浊流沉积特征——以达49井为例[J]. 石油学报, 2017, 38(7): 777-792.

Gao Hongcan, Zheng Rongcai, Xiao Bin, Liu Yun, Zheng Ling, Luan Yanchun, Liu Hongli. Slump-turbidite sedimentary characteristics of the Lower Cretaceous Tenggeer Formation in Baiyinchagan sag of Erlian Basin:a case study of Well Da 49[J]. Acta Petrolei Sinica, 2017, 38(7): 777-792.

参考文献

[1] 何起祥,刘招君,王东坡,等.湖泊相浊积岩的主要特征及其地质意义[J].沉积学报,1984,2(4):33-46.
HE Qixiang,LIU Zhaojun,WANG Dongpo,et al.Characteristics of lacustrine turbidites and their tectonic significance[J].Acta Sedimentologica Sinica,1984,2(4):33-46.
[2] 李文厚,邵磊,魏红红,等.西北地区湖相浊流沉积[J].西北大学学报:自然科学版,2001,31(1):57-62.
LI Wenhou,SHAO Lei,WEI Honghong,et al.Turbidity current deposits of lake facies in northwestern China[J].Journal of Northwest University:Natural Science Edition,2001,31(1):57-62.
[3] 李文厚,周立发,符俊辉,等.库车坳陷上三叠统的浊流沉积及石油地质意义[J].沉积学报,1997,15(1):20-24.
LI Wenhou,ZHOU Lifa,FU Junhui,et al.Turbidity current deposits and their significance for petroleum geology of Upper Triassic in the Kuqa depression[J].Acta Sedimentologica Sinica,1997,15(1):20-24.
[4] 饶孟余,钟建华,郭泽清,等.济阳坳陷牛庄洼陷沙三段三角洲前缘浊积岩特征[J].高校地质学报,2004,10(4):624-633.
RAO Mengyu,ZHONG Jianhua,GUO Zeqing,et al.Turbidite characteristics of delta front for the 3rd member of Shahejie Formation in Niuzhuang sag,Jiyang depression[J].Geological Journal of China Universities,2004,10(4):624-633.
[5] 张光亚,马锋,梁英波,等.全球深层油气勘探领域及理论技术进展[J].石油学报,2015,36(9):1156-1166.
ZHANG Guangya,MA Feng,LIANG Yingbo,et al.Domain and theory-technology progress of global deep oil & gas exploration[J].Acta Petrolei Sinica,2015,36(9):1156-1166.
[6] 吴崇筠.湖盆砂体类型[J].沉积学报,1986,4(4):1-27.
WU Chongyun.Sandbodies in lake basin[J].Acta Sedimentologica Sinica,1986,4(4):1-27.
[7] 姜涛,解习农.细粒浊积体的油气地质意义[J].地质科技情报,2003,22(2):51-55.
JIANG Tao,XIE Xinong.Hydrocarbon value of fine-grained turbidite systems[J].Geological Science and Technology Information,2003,22(2):51-55.
[8] 郑荣才,文华国,韩永林,等.鄂尔多斯盆地白豹地区长6油层组湖底滑塌浊积扇沉积特征及其研究意义[J].成都理工大学学报:自然科学版,2006,33(6):566-575.
ZHENG Rongcai,WEN Huaguo,HAN Yonglin,et al.Discovery and significance of sublacustrine slump turbidite fans in Chang 6 oil-bearing Formation of Baibao region in Ordos Basin,China[J].Journal of Chengdu University of Technology:Science & Technology Edition,2006,33(6):566-575.
[9] 于俊峰,裴健翔,王立锋,等.莺歌海盆地东方13-2重力流储层超压气田气藏性质及勘探启示[J].石油学报,2014,35(5):829-838.
YU Junfeng,PEI Jianxiang,WANG Lifeng,et al.Gas pool properties and its exploration implications of the Dongfang 13-2 gravity reservoir-overpressure gas field in Yinggehai Basin[J].Acta Petrolei Sinica,2014,35(5):829-838.
[10] 朱筱敏,信荃麟,刘泽容.陆相断陷湖盆中滑塌浊积扇的识别[J].科学通报,1991,36(7):535-537.
ZHU Xiaomin,XIN Quanlin,LIU Zerong.Recognition of the slumping turbidite fans in down-faulted lacustrine basins[J].Chinese Science Bulletin,1991,36(20):1715-1719.
[11] 德勒恰提·加娜塔依,张明玉,陈春勇,等.准噶尔盆地吉木萨尔凹陷东部二叠系梧桐沟组湖底扇沉积特征及展布[J].石油学报,2015,36(6):688-698.
DELEQIATI Janney,ZHANG Mingyu,CHEN Chunyong,et al.Sedimentary characteristics and distribution of sublacustrine fan in Permian Wutonggou Formation,eastern Jimsar sag,Junggar Basin[J].Acta Petrolei Sinica,2015,36(6):688-698.
[12] 贾承造,庞雄奇.深层油气地质理论研究进展与主要发展方向[J].石油学报,2015,36(12):1457-1469.
JIA Chengzao,PANG Xiongqi.Research processes and main development directions of deep hydrocarbon geological theories[J].Acta Petrolei Sinica,2015,36(12):1457-1469.
[13] 周庆凡.浊流沉积体系与油气勘探[J].国外油气勘探,1994,6(3):288-297.
ZHOU Qingfan.Turbidite sedimentary systems and petroleum exploration[J].Oil & Gas Prospecting Abroad, 1994,6(3):288-297.
[14] 彭大均,陈长民,庞雄,等.南海珠江口盆地深水扇系统的发现[J].石油学报,2004,25(5):17-23.
PENG Dajun,CHEN Changmin,PANG Xiong,et al.Discovery of deep-water fan system in South China Sea[J].Acta Petrolei Sinica,2004,25(5):17-23.
[15] 李云,郑荣才,朱国金,等.珠江口盆地荔湾3-1气田珠江组深水扇沉积相分析[J].沉积学报,2011,29(4):665-676.
LI Yun,ZHENG Rongcai,ZHU Guojin,et al.Facies and depositional model of a deepwater fan in the Zhujiang formation,Liwan 3-1 Gasfield,Baiyun Sag,Pearl River Mouth Basin[J].Acta Sedimentologica Sinica,2011,29(4):665-676.
[16] 郑荣才,郑哲,高博禹,等.珠江口盆地白云凹陷珠江组海底扇深水重力流沉积特征[J].岩性油气藏,2013,25(2):1-8.
ZHENG Rongcai,ZHENG Zhe,GAO Boyu,et al.Sedimentary features of the gravity flows in submarine fan of Zhujiang Formation in Baiyun sag,Pearl River Mouth Basin[J].Lithologic Reservoirs,2013,25(2):1-8.
[17] 高红灿,肖斌,郑荣才,等.白音查干凹陷下白垩统腾格尔组砾质滩坝沉积特征[J].石油与天然气地质,2015,36(4):612-620.
GAO Hongcan,XIAO Bin,ZHENG Rongcai,et al.Sedimentary characteristics of gravelly beach-bar in the Lower Cretaceous Tenggeer Formation of Baiyinchagan sag,Erlian Basin[J].Oil & Gas Geology,2015,36(4):612-620.
[18] KUENEN P H,MIGLIORINI C I.Turbidity currents as a cause of graded bedding[J].The Journal of Geology,1950,58(2):91-127.
[19] BOUMA A H.Sedimentology of some flysch deposits:a graphic approach to facies interpretation[M].Amsterdam:Elsevier,1962:88-123.
[20] SANDERS J E.Primary sedimentary structures formed by turbidity currents and related resedimentation mechanisms[C]//MIDDLETON G V.Primary Sedimentary Structures and their Hydrodynamic Interpretation.Tulsa,Oklahoma:SEPM Special Publication 12,1965:192-219.
[21] MIDDLETON G V,HAMPTON M A.Sediment gravity flows:Mechanics of flow and deposition[C]//MIDDLETON G V,BOUMA A H.Turbidites and Deep-Water Sedimentation.Los Angeles,California:SEPM Pacific Section,1973:1-38.
[22] DOTT R H.Dynamics of subaqueous gravity depositional processes[J].AAPG Bulletin, 1963,47(1):104-128.
[23] 高红灿,郑荣才,魏钦廉,等.碎屑流与浊流的流体性质及沉积特征研究进展[J].地球科学进展,2012,27(8):815-827.
GAO Hongcan,ZHENG Rongcai,WEI Qinlian,et al.Reviews on fluid properties and sedimentary characteristics of debris flows and turbidity currents[J].Advances in Earth Science,2012,27(8):815-827.
[24] MUTTI E.Turbidite sandstones[M].Milan,Italy:AGIP Special Publication,1992:1-275.
[25] KNELLER B.When is a turbidity current not a turbidity current? A question of mobility[C]//AAPG 1996 Annual Meeting Abstracts.Tulsa,Oklahoma:AAPG,1996:76.
[26] MUTTI E,TINTERRI R,REMACHA E,et al.An introduction to the analysis of ancient turbidite basins from an outcrop perspective[C]//AAPG Continuing Education Course Note Series.Tulsa,Oklahoma:AAPG,1999:61.
[27] SHANMUGAM G.High-density turbidity currents; are they sandy debris flows[J].Journal of Sedimentary Research,1996,66(1):2-10.
[28] SHANMUGAM G.The Bouma sequence and the turbidite mind set[J].Earth-Science Reviews,1997,42(4):201-229.
[29] SHANMUGAM G.Ten turbidite myths[J].Earth-Science Reviews,2002,58(3/4):311-341.
[30] SHANMUGAM G.50 years of the turbidite paradigm (1950s-1990s):deep-water processes and facies models-a critical perspective[J].Marine and Petroleum Geology,2000,17(2):285-342.
[31] SHANMUGAM G.Deep-water processes and facies models:implications for sandstone petroleum reservoirs[M].New York:Elsevier,2006:1-456.
[32] 张福顺,樊太亮,王生朗,等.白音查干凹陷层序地层格架及充填样式[J].地球学报,2003,24(2):137-142.
ZHANG Fushun,FAN Tailiang,WANG Shenglang,et al.The sequence stratigraphic framework and the filling style of Baiyinchagan depression[J].Acta Geoscientia Sinica,2003,24(2):137-142.
[33] 许书堂,马维民,王德仁,等.二连盆地白音查干凹陷下白垩统层序地层研究[J].沉积学报,2004,22(4):644-650.
XU Shutang,MA Weimin,WANG Deren,et al.Sequence strata of lower cretaceous in Baiyinchagan depression,Erlian Basin[J].Acta Sedimentologica Sinica,2004,22(4):644-650.
[34] 邓已寻,杨丽英,张梅,等.白音查干凹陷达尔其油田油藏特征与勘探潜力[J].大庆石油地质与开发,2004,23(4):7-10.
DENG Yixun,YANG Liying,ZHANG Mei,et al.Geologic characteristics of oil reservoirs and exploration potential of Daerqi oilfield in Baiyinchagan sag[J].Petroleum Geology & Oilfield Development in Daqing,2004,23(4):7-10.
[35] 周连德,徐国盛,王威.白音查干凹陷达尔其油田沉积相与油(气)分布[J].物探化探计算技术,2007,29(5):405-410.
ZHOU Liande,XU Guosheng,WANG Wei.Sedimentary facies and petroleum distribution in Daerqi oilfield,Baiyinchagan sag[J].Computing Techniques for Geophysical and Geochemical Exploration,2007,29(5):405-410.
[36] 岳信东,林春明,李艳丽,等.二连盆地白音查干凹陷下白垩统腾格尔组沉积相[J].沉积学报,2008,26(4):593-601.
YUE Xindong,LIN Chunming, LI Yanli,et al.Sedimentary facies in the early cretaceous Tenggeer formation of Baiyinchagan depression,Erlian Basin[J].Acta Sedimentologica Sinica, 2008,26(4):593-601.
[37] 林春明,张志萍,李艳丽,等.二连盆地白音查干凹陷早白垩世腾格尔组沉积特征及物源探讨[J].高校地质学报,2009,15(2):226-239.
LIN Chunming,ZHANG Zhiping,LI Yanli,et al.Sedimentary characteristics and source provenance in the early cretaceous Tenggeer Formation of Baiyinchagan sag,Erlian Basin[J].Geological Journal of China Universities,2009,15(2):226-239.
[38] 王先德.二连盆地白音查干凹陷下白垩统巴彦花群沉积特征与油气藏预测[D].北京:中国地质大学(北京),2011:39-78.
WANG Xiande.The study of depositional characteristics and the prediction of oil and gas reservoirs in Bayanhua Group of the Lower Cretaceous in Baiyinchagan Depression of Erlian Basin[D].Beijing:China University of Geosciences (Beijing),2011:39-78.
[39] 高红灿,谭先锋,况昊.二连盆地白音查干凹陷下白垩统腾格尔组层序地层:2015年全国沉积学大会沉积学与非常规资源论文摘要集[C].武汉:长江大学、中国地质大学(武汉),2015,107. GAO Hongcan,TAN Xianfeng,KUANG Hao.Sequence stratigraphy of the Early Cretaceous Tenggeer Formation of Baiyinchagan sag, Erlian Basin:China Sedimentary Conference of Sedimentology and Unconventional Resources[C].Wuhan:Yangtze University & China University of Geosciences(Wuhan),2015,107.
[40] 解吉高,刘春成,刘志斌,等.下刚果盆地北部中新统深水浊积岩储层及含油性地震预测[J].石油学报,2015,36(1):33-40.
XIE Jigao,LIU Chuncheng,LIU Zhibin,et al.Seismic prediction of the reservoir and oil-bearing property of Miocene deep-water turbidite in northern Lower Congo Basin[J].Acta Petrolei Sinica,2015,36(1):33-40.
[41] 肖斌,陈发亮,郑玲,等.白音查干凹陷岩性圈闭预测描述与评价技术[R].濮阳:中国石化中原油田分公司物探研究院,2013.
XIAO Bin,CHEN Faliang,ZHENG Ling,et al.Prediction,description and evaluation technology for lithologic traps in Baiyinchagan sag[R].Puyang:Sinopec Geophysical Research Institute of Zhongyuan Oilfield Company,2013.
[42] SHANMUGAM G.深水砂体成因研究新进展[J].石油勘探与开发,2013,40(3):294-301.
SHANMUGAM G.New perspectives on deep-water sandstones:implications[J].Petroleum Exploration and Development,2013,40(3):294-301.
[43] MOSCARDELLI L,WOOD L,MANN P.Mass-transport complexes and associated processes in the offshore area of Trinidad and Venezuela[J].AAPG Bulletin,2006,90(7):1059-1088.
[44] POSAMENTIER H W,MARTINSEN O J.The character and genesis of submarine mass-transport deposits:insights from outcrop and 3D seismic data[C]//SHIPP R C,WEIMER P,POSAMENTIER H W.Mass-Transport Deposits in Deepwater Settings.Tulsa,Oklahoma:SEPM Special Publication,2011:7-38.
[45] HARMS J C,FAHNESTOCK R K.Stratification,bed forms,and flow phenomena (with an example from the Rio Grande)[C]//MIDDLETON G V.Primary Sedimentary Structures and Their Hydrodynamic interpretation.Tulsa,Oklahoma:SEPM Special Publication 12,1965:84-115.
[46] KUENEN P H.Emplacement of flysch-type sand beds[J].Sedimentology,1967,9(3):203-243.
[47] MIDDLETON G V.Experiments on density and turbidity currents:Ⅲ.Deposition of sediment[J].Canadian Journal of Earth Sciences,1967,4(3):475-505.
[48] BATES R L,JACKSON J A.Glossary of geology[M].2nd ed.Virginia:American Geological Institute,1980:751.
[49] 袁静,梁绘媛,梁兵,等.湖相重力流沉积特征及发育模式——以苏北盆地高邮凹陷深凹带戴南组为例[J].石油学报,2016,37(3):348-359.
YUAN Jing,LIANG Huiyuan,LIANG Bing,et al.Sedimentary characteristics and development model of lacustrine gravity flow:a case study of Dainan Formation in deep sag belt of Gaoyou depression,Northern Jiangsu Basin[J].Acta Petrolei Sinica,2016,37(3):348-359.
[50] 李存磊,任伟伟,唐明明.流体性质转换机制在重力流沉积体系分析中应用初探[J].地质论评,2012,58(2):285-296.
LI Cunlei,REN Weiwei,TANG Mingming.Preliminary study on gravity flow depositional system based on fluid properties conversion theory[J].Geological Review,2012,58(2):285-296.
[51] 庞雄,朱明,柳保军,等.南海北部珠江口盆地白云凹陷深水区重力流沉积机理[J].石油学报,2014,35(4):646-653.
PANG Xiong,ZHU Ming,LIU Baojun,et al.The mechanism of gravity flow deposition in Baiyun sag deepwater area of the northern South China Sea[J].Acta Petrolei Sinica,2014,35(4):646-653.
[52] TALLING P J,AMY L A,WYNN R B,et al.Beds comprising debrite sandwiched within co-genetic turbidite:origin and widespread occurrence in distal depositional environments[J].Sedimentology,2004,51(1):163-194.
[53] FELIX M,PEAKALL J.Transformation of debris flows into turbidity currents:mechanisms inferred from laboratory experiments[J].Sedimentology,2006,53(1):107-123.
[54] HAUGHTON P,DAVIS C,MCCAFFREY W,et al.Hybrid sediment gravity flow deposits-classification,origin and significance[J].Marine and Petroleum Geology,2009,26(10):1900-1918.
[55] 杨田,操应长,王艳忠,等.深水重力流类型、沉积特征及成因机制——以济阳坳陷沙河街组三段中亚段为例[J].石油学报,2015,36(9):1048-1059.
YANG Tian,CAO Yingchang,WANG Yanzhong,et al.Types,sedimentary characteristics and genetic mechanisms of deep-water gravity flows:a case study of the middle submember in Member 3 of Shahejie Formation in Jiyang depression[J].Acta Petrolei Sinica,2015,36(9):1048-1059.
[56] 方爱民,李继亮,侯泉林.浊流及相关重力流沉积研究综述[J].地质论评,1998,44(3):270-280.
FANG Aimin,LI Jiliang,HOU Quanlin.Sedimentation of turbidity currents and relative gravity flows:a review[J].Geological Review,1998,44(3):270-280.
[57] 张传恒,武振杰,高林志,等.华北中元古界雾迷山组地震驱动的软沉积物变形构造及其地质意义[J].中国科学D辑:地球科学,2007,37(3):336-343.
ZHANG Chuanheng,WU Zhenjie,GAO Linzhi,et al.Soft sediment deformation structure by earthquake and its geological significance in Mesoproterozoic mishan group of Huabei[J].Science in China Series D:Earth Sciences,2007,50(3):350-358.
[58] 李磊,王英民,徐强,等.南海北部白云凹陷21 Ma深水重力流沉积体系[J].石油学报,2012,33(5):798-806.
LI Lei,WANG Yingmin,XU Qiang,et al.21 Ma deepwater gravity flow depositional system in Baiyun sag,northern South China Sea[J].Acta Petrolei Sinica,2012,33(5):798-806.
[59] READING H G,RICHARDS M.Turbidite systems in deep-water basin margins classified by grain size and feeder system[J].AAPG Bulletin,1994,78(5):792-822.
[60] 刘立,曹林,徐开志.深水浊积体系的成因类型及其与海(湖)平面升降的关系[J].世界地质,1995,14(4):8-12.
LIU Li,CAO Lin,XU Kaizhi.Genetic type of deep water turbidite system and the relationship with sea-level change[J].Global Geology,1995,14(4):8-12.
[61] 刘招君,王东坡,何起祥.攀西地区上三叠统湖泊浊积岩沉积特征及其地质意义[C]//张云湘.中国攀西裂谷文集.北京:地质出版社,1985:298-306.
LIU Zhaojun,WANG Dongpo,HE Qixiang.Sedimentary character and geological significance of Upper Triassic lake facies turbidite in Panxi area[C]//ZHANG Yunxiang.Contribution to Panxi Rift China.Beijing:Geological Publishing House,1985:298-306.
[62] 刘宪斌,万晓樵,林金逞,等.陆相浊流沉积体系与油气[J].地球学报,2003,24(1):61-66.
LIU Xianbin,WAN Xiaoqiao,LIN Jincheng,et al.Continental turbidite deposition system and hydrocarbon[J].Acta Geoscientia Sinica,2003,24(1):61-66.
[63] 方勇,邓宏文,王红亮,等.东营三角洲高频层序特征与岩性圈闭分布[J].中国海上油气(地质),2003,17(3):160-163.
FANG Yong,DENG Hongwen,WANG Hongliang,et al.High frequency sequence and lithologic trap distribution in Dongying delta[J].China Offshore Oil and Gas (Geology),2003,17(3):160-163.
[64] 张伟,刘建朝,高志亮,等.鄂尔多斯盆地吴堡地区长6段浊积特征及其石油地质意义[J].地球科学与环境学报,2012,34(2):64-71.
ZHANG Wei,LIU Jianchao,GAO Zhiliang,et al.Turbidity characteristics and petroleum geological significance of Chang-6 Section in Wubu area of Ordos Basin[J].Journal of Earth Sciences and Environment,2012,34(2):64-71.
[65] 石玉江,李文厚,王长胜,等.鄂尔多斯盆地三叠系延长组长7段浊积扇对油气聚集的控制[J].地质通报,2016,35(2/3):406-414.
SHI Yujiang,LI Wenhou,WANG Changsheng,et al.Turbidite fan and its controlling effects on hydrocarbon accumulation in the Chang 7 Member of Triassic Yanchang Formation in Ordos Basin[J].Geological Bulletin of China,2016,35(2/3):406-414.
[66] 尹太举,张昌民,李中超.东营凹陷滑塌浊积岩沉积特征及油气藏勘探技术[J].石油与天然气地质,2006,27(1):93-98.
YIN Taiju,ZHANG Changmin,LI Zhongchao.Depositonal characteristics of fluxoturbidite and exploration technologics of subtle reservoirs in the Dongying sag[J]. Oil & Gas Geology,2006,27(1):93-98.
[67] 李丕龙.陆相断陷盆地油气地质与勘探(卷二):陆相断陷盆地沉积体系与油气分布[M].北京:石油工业出版社,2003:20-50,58-69.
LI Pilong.Petroleum geology and exploration of continental fault basin(Volume 2):sedimentary system and hydrocarbon distribution of continental fault basin[M].Beijing:Petroleum Industry Press,2003:20-50,58-69.
[68] 丁桔红.湖盆浊积砂体及类型研究[J].华南地质与矿产,2007(3):6-11.
DING Juhong.Researching of the turbidity sand body and types in the lake basin[J].Geology and Mineral Resources of South China,2007(3):6-11.
[69] 祝杰,李野.滨南油田沙三段浊积砂体沉积特征与有利储集相带分析[J].辽宁化工,2015,44(10):1232-1236.
ZHU Jie,LI Ye.Sedimentary characteristics and favorable reservoir facies of E₂s₃ Formation in Binnan oilfield[J].Liaoning Chemical Industry,2015,44(10):1232-1236.
[70] 董艳蕾,朱筱敏,耿晓洁,等.利用地层切片研究陆相湖盆深水滑塌浊积扇沉积特征[J].地学前缘,2015,22(1):386-396.
DONG Yanlei,ZHU Xiaomin,GENG Xiaojie,et al.Using the stratal slice to study the depositional characteristics of deep-water slumped turbidite fans in continental lake basin[J].Earth Science Frontiers,2015,22(1):386-396.
[71] 鄢继华,陈世悦,宋国奇,等.三角洲前缘滑塌浊积岩形成过程初探[J].沉积学报,2004,22(4):573-578.
YAN Jihua,CHEN Shiyue,SONG Guoqi,et al.Preliminary study on the formation of fluxoturbidite in front of delta[J].Acta Sedimentologica Sinica,2004,22(4):573-578.
[72] 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.Simulation of luxoturbidite in front of delta[J].Acta Sedimentologica Sinica,2006,24(1):50-55.
[73] 刘招君.湖泊水下扇沉积特征及影响因素——以伊通盆地莫里青断陷双阳组为例[J].沉积学报,2003,21(1):148-154.
LIU Zhaojun.Lacus Subaqueous fan sedimentary characteristics and influence factor-a case study of Shuangyang Formation in Moliqing fault subsidence of Yitong Basin[J].Acta Sedimentologica Sinica,2003,21(1):148-154.
[74] 王东坡,刘立,张立平,等.松辽盆地白垩纪古气候沉积旋回层序地层[M].长春:吉林大学出版社,1995:1-202.
WANG Dongpo,LIU Li,ZHANG Liping,et al.Palaeoclimatology,sedimentary cycle,sequence stratigraphy of Cretaceous in Songliao Basin[M].Changchun:Jilin University Press,1995:1-202.
[75] 郭佳,邓宏文,王红亮.松南西斜坡三角洲前缘-滑塌浊积岩沉积相及展布规律[J].地球科学-中国地质大学学报,2011,36(6):1095-1104.
GUO Jia,DENG Hongwen,WANG Hongliang.Sedimentary facies and distribution of delta front-fluxoturbidite in the western slope of south Songliao Basin[J].Earth Science-Journal of China University of Geosciences,2011,36(6):1095-1104.
[76] 刘立,曹林,徐开志,等.莫里青断陷西部双阳组(始新世)的浊积扇沉积特征[J].长春地质学院学报,1996,26(3):261-264.
LIU Li,CAO Lin,XU Kaizhi,et al.The sedimentary characteristics of the turbidite fans in Shuangyang Formation (Eocene),the western Moliqing Fault Basin[J].Journal of Changchun University of Earth Sciences,1996,26(3):261-264.
[77] ROSS W C,HALLIWELL B A,MAY J A,et al.Slope readjustment:a new model for the development of submarine fans and aprons[J].Geology,1994,22(6):511-514.
[78] 魏魁生,徐怀大.二连盆地白垩系非海相沉积层序地层特征[J].地球科学-中国地质大学学报,1994,19(2):181-193.
WEI Kuisheng,XU Huaida.Sequence stratigraphic features of Cretaceous nonmarine sediments in Erlian Basin[J].Earth Science-Journal of China University of Geosciences,1994,19(2):181-193.
[79] 王东坡,刘立.大陆裂谷盆地层序地层学的研究[J].岩相古地理,1994,14(3):1-9.
WANG Dongpo,LIU Li.Sequence stratigraphy in continental rift basins[J].Sedimentary Facies and Palaeogeography,1994,14(3):1-9.
[80] 宋国奇.济阳坳陷下第三系湖相沉积的层序地层学分析[J].现代地质,1993,7(1):20-29.
SONG Guoqi.Sequence stratigraphic analysis of Eogene system lacustrine deposit in Jiyang depression[J].Geoscience,1993,7(1):20-29.
[81] 孙德有,高福红,付长亮,等.白音查干凹陷腾格尔组和阿二段储层微观特征研究[R].长春:吉林大学地球科学学院,2008.
SUN Deyou,GAO Fuhong,FU Changliang,et al.Research on reservoir microscopic characteristics of 2nd Member of Aershan Formation and Tengge'er Formation in Baiyinchagan sag[R].Changchun:College of Earth Sciences,Jilin University,2008.

二连盆地白音查干凹陷下白垩统腾格尔组滑塌-浊流沉积特征——以达49井为例

Slump-turbidite sedimentary characteristics of the Lower Cretaceous Tenggeer Formation in Baiyinchagan sag of Erlian Basin:a case study of Well Da 49

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