天然气地球科学
高级检索
作者投稿 专家审稿 编辑办公

天然气地球科学

• 天然气地质学 • 上一篇    下一篇

松辽盆地坳陷期湖底扇沉积特征与分布规律——以英台地区青山口组为例

张庆石，张革，陈彬滔，王革，梁苏娟，刘彩燕   

  1. 1.成都理工大学沉积地质研究院，四川 成都 610059；
    2.中国石油大庆油田有限责任公司勘探开发研究院,黑龙江 大庆 163712；
    3.中国石油勘探开发研究院西北分院，甘肃 兰州 730020
  • 收稿日期:2013-04-22 修回日期:2013-10-29 出版日期:2014-03-10 发布日期:2014-03-10
  • 通讯作者: 张庆石zqshi@petrochina.com.cn E-mail:zqshi@petrochina.com.cn
  • 作者简介:张庆石(1968-),男,辽宁法库人,高级工程师,博士研究生，主要从事油气勘探研究.E-mail：zqshi@petrochina.com.cn.
  • 基金资助:

    国家科技重大专项(编号：2011ZX05007-002)；中国石油天然气股份有限公司重大专项“松辽盆地北部致密砂岩油和泥(页)岩油资源潜力及富集规律研究”(编号：2012E-2603-01)联合资助.

Deposition Characteristics and Distribution Pattern of Sublaucustrine Fan in Qingshankou Formation,Songliao Basin

ZHANG Qing-Shi，ZHANG Ge，CHEN Bin-Tao，WANG Ge，LIANG Su-Juan，LIU Cai-Yan   

  1. 1.Sedimentary Institute of Chengdu University of Technology,Chengdu 610059,China;
    2.Daqing Oil Field Company,CNPC,Daqing 163712,China;3.Northwest Branch of Research Institute of Petroleum 
    Exploration and Development,PetroChina,Lanzhou 730020,China
  • Received:2013-04-22 Revised:2013-10-29 Online:2014-03-10 Published:2014-03-10

PDF (PC)

647

摘要：

湖底扇是源内油气藏勘探的重要领域。选取松辽盆地西部坡折带重力流为研究对象，利用岩心、测井和地震资料，对大型坳陷湖盆坡折带背景下湖底扇的形成条件、沉积特征、地震响应和分布规律进行研究。湖盆古地形恢复表明，英台地区为坡折带背景，坡折带是重力流卸载的重要场所，同沉积断裂运动、地震活动、火山喷发为重力流的形成提供了触发机制。湖底扇主要由砂质碎屑流、滑动岩和滑塌岩等块体搬运体组成，浊积岩极为少见。湖底扇具有敏感的地震响应特征，剖面上为透镜状，内部振幅和频率变化较大。湖底扇主要分布在四级旋回的基准面上升期，平面上在扇三角洲前缘外侧连片分布，油气成藏条件优越，是岩性油气藏勘探的有利目标。

关键词: 湖底扇, 重力流, 块体搬运体, 浊积岩, 松辽盆地

Abstract:

blacustrine fan is an important field for oil & gas exploration within source rock.Based on core,logging,and 3D seismic data,formation condition,sedimentary characteristics,seismic responses,and distribution pattern of sublacustrine fan in west slope break zone of Songliao Basin have been studied.The results of paleotopography reconstruction show that slope break zone is well developed in Yingtai area.Furthermore,slope break zone is an important discharging place for gravity flow sediments.Syndepositional fault movement,earthquake activity,and volcanic eruption are major trigger mechanisms for the formation of gravity flow.Sublacustrine fan is mainly composed of sandy debrite,sandy slide and sandy slump,with rare turbidite.Meanwhile,sublacustrine fan has sensitive seismic response characteristics,which is characterized by lenticular external configuration with varied internal amplitude and frequency in seismic profile.Sublacustrine fan is mainly distributed in the rising stage of forth-order base level cycle in vertical and adjacent to fan delta front in plane.On the whole,sublacustrine fan is characterized by excellent hydrocarbon accumulation condition,which can be a favorable target for lithologic reservoir exploration.

Key words: Sublacustrine fan, Gravity flow, Mass-transport deposits, Turbidite, Songliao Basin

中图分类号: 

  • TE121.3

［1］Chen Guangpo,Wang Tianqi,Li Linbo,et al.Characteristics of sublacustrine fan in half-graben rift lake basin and its petroleum prospecting:Case study on the second member of Tenggeer Formation,Saihantala Sag,Erlian Basin［J］.Petroleum Exploration and Development,2010,37(1):63-69.［陈广坡,王天琦,李林波,等.箕状断陷湖盆湖底扇特征及油气勘探——以二连盆地赛汉塔拉凹陷腾格尔组二段为例［J］.石油勘探与开发,2010,37(1):63-69.］

［2］Deng Yilin,Wang Tianqi,Cao Zhenglin,et al.Depositional characteristics and genesis of Lower  Cretaceous sublacustrine fan in Wuliyast Sag,Erlian Basin［J］.Natural Gas Geoscience,2010,21(5):786-792.［邓毅林,王天琦,曹正林,等.二连盆地乌里雅斯太凹陷下白垩统湖底扇沉积特征及成因分析［J］.天然气地球科学,2010,21(5):786-792.］

［3］Li Yun,Zheng Rongcai,Gao Boyu,et al.Reviews and prospects on submarine fan deposition：A case study of Zhujiang submarine fan system in Baiyun Depression,Pearl River Mouth Basin［J］.Geological Review,2010,56(4):549-560.［李云,郑荣才,高博禹,等.深水扇沉积研究现状和展望——以珠江口盆地白云凹陷珠江深水扇系统为例［J］.地质论评,2010,56(4):549-560.］

［4］Mo Wuling,Wu Chaodong,Zhang Shun.Generation mechanism of sediment gravity flow of Nenjiang Formation in the north Songliao Basin［J］.Natural Gas Geoscience,2013,24(3):555-565.［莫午零,吴朝东,张顺.松辽盆地北部嫩江组沉积物重力流形成机制［J］.天然气地球科学,2013,24(3):555-565.］[JP]

［5］Wang Jiangong,Wang Tianqi,Zhang Shun,et al.Sedimentary characteristics and geophysical response of sublacustrine fan during transgress period in Songliao Basin［J］.Acta Petrolei Sinica,2009,30(3):361-366.［王建功,王天琦,张顺,等.松辽坳陷盆地水侵期湖底扇沉积特征及地球物理响应［J］.石油学报,2009,30(3):361-366.］

［6］Lu Zhiyong.Sedimentary characteristics and model of gravity flows in Yan 18 area of the steep slope in Dongying Sag of Jiyang Depression［J］.Natural Gas Geoscience,2012,23(3):420-429.［路智勇.济阳坳陷东营凹陷陡坡带盐18地区重力流沉积特征与沉积模式［J］.天然气地球科学,2012,23(3):420-429.］ 

［7］Pan Shuxin,Zheng Rongcai,Wei Pingsheng,et al.Deposition characteristics,recognition mark and form mechanism of mass transport deposits in terrestrial lake basin［J］.Lithologic Reservoirs,2013,25(2):9-18.［潘树新,郑荣才,卫平生,等.陆相湖盆块体搬运体的沉积特征、识别标志与形成机制［J］.岩性油气藏,2013,25(2):9-18.］

［8］Shanmugam G.Ten turbidite myths［J］.Earth Science Reviews,2002,58(3):311-341.

［9］Wang Lan,Zou Caineng,Lin Tong,et al.Sedimentary environment and diagenesis facies of Chang 6 Yanchang Formation in Baibao-Huachi,Ordos Basin［J］.Natural Gas Geoscience,2011,22(5):796-806.［王岚,邹才能,林潼,等.鄂尔多斯盆地白豹—华池地区延长组长6油层组沉积环境及成岩相分析［J］.天然气地球科学,2011,22(5):796-806.］

［10］Posamentier H W,Martinsen O J.The character and genesis of submarine mass-transport deposits:Insights from outcrop and 3D seismic data［C］//SEPM Special Publication,96 Tulsa OK.Society for Sedimentary Geology,2011:7-38.[JP]

［11］Li Changsong,Pan Yuanlin,Xiao Jianxin,et al.Structural slope-break zone:key concept for stratigraphic sequence analysis and petroleum forecasting in fault subsidence basins［J］.Earth Science:Journal of China University of Geosciences,2000,25(3):260-266.［林畅松,潘元林,肖建新,等.“构造坡折带”——断陷盆地层序分析和油气预测的重要概念［J］.地球科学,2000,25(3):260-266.］

［12］Wang Yingmin,Jin Wudi,Liu Shuhui,et al.Genetic types,distribution and exploration significance of multistage slope breaks in rift lacustrine basin［J］.Oil & Gas Geology,2003,24(6):199-203.214.［王英民,金武弟,刘书会,等.断陷湖盆多级坡折带的成因类型、展布及其勘探意义［J］.石油与天然气地质,24(6):199-203,214.］

［13］Deng Hongwen,Wang Hongliang,Wang Dunze.Control of paleo-morphology to stratigraphic sequence in continental rift basins:Take lower tertiary of western slope in Bozhong Depression as an example［J］.Oil & Gas Geology,2001,22(4):293-296,303.［邓宏文,王红亮,王敦则.古地貌对陆相裂谷盆地层序充填特征的控制——以渤中凹陷西斜坡区下第三系为例［J］.石油与天然气地质,2001,22(4):293-296,303.］

［14］Feng Youliang,Xu Xiusheng.Syndepositional structural slope-break zone controls on lithologic reservoirs：A case from Paleogene Bohai Bay Basin［J］.Petroleum Exploration and Development,2006,33(1):22-25，31.［冯有良,徐秀生.同沉积构造坡折带对岩性油气藏富集带的控制作用——以渤海湾盆地古近系为例［J］.石油勘探与开发,2006(01):22-25，31.］

［15］Huang Wei,Wang Jiangong,Zhao Yingcheng,et al.Characteristics of slope break in depression stage of Songliao Basin［J］.Acta Petrolei Sinica,2007,28(4):31-35.［黄薇,王建功,赵应成,等.松辽盆地拗陷期坡折带特征［J］.石油学报,2007,28(4):31-35.］

［16］Wei Pingsheng,Pan Shuxin,Wang Jiangong,et al.Study of the relationship between lithostratigraphic reservoirs and lakeshore line:Introduction on lakeshore line controlling oil/gas reservoirs in sag basin［J］.Lithologic reservoirs,2007,19(1):27-32.［卫平生,潘树新,王建功,等.湖岸线和岩性地层油气藏的关系研究——论“坳陷盆地湖岸线控油”［J］.岩性油气藏,2007,19(1):27-32.］

［17］Wang Dongpo,Liu Zhaojun,Liu Li.Evolution of Songliao Basin and Sea Level Fluctuation［M］.Beijing:Geological Publishing House,1994.［王东坡,刘招君,刘立.松辽盆地演化与海平面升降［M］.北京：地质出版社,1994.］

［18］Pan Shuxin,Wei Pingsheng,Wang Tianqi,et al.Discovery of easten provenance in Songliao Basin and its implications on petroleum geology［J］.Natural Gas Geoscience,2011,22(6):1021-1027.［潘树新,卫平生,王天琦,等.松辽盆地东部物源的发现及其石油地质意义［J］.天然气地球科学,2011,22(6):1021-1027.］[JP]

［19］Pan Shuxin,Wang Jiangong,Liu Caiyan,et al.Sedimentary features,distribution pattern and accumulation mechanism of lake shore bar:Taking the Qingshankou Formation in the southern Songliao Basin as an example［J］.Journal of Jilin University:Earth Science Edition,2012,42(supplement 2):70-78.［潘树新,王建功,刘彩燕,等.坳陷湖盆沿岸坝沉积特征、分布规律及成藏机制——以松辽盆地南部青山口组为例［J］.吉林大学学报：地球科学版,2012,42(增刊2):70-78.］

［20］Kang Bo,Xie Xinong,Du Xuebin,et al.A New paleobathymetric approach based on shoreline trajectory:An example from Dongying delta in the third member of Paleogene Shahejie Formation［J］.Acta Sedimentologica Sinica,2012,30(3):443-450.［康波,解习农,杜学斌,等.基于滨线轨迹的古水深定量计算新方法——以古近系沙三中段东营三角洲为例［J］.沉积学报,2012,30(3):443-450.］

［21］Kang An,Zhu Xiaomin,Wang Guiwen,et al.Application of paleobathymetric curve in the sequence stratigraphy of well-logging data［J］.Acta Sedimentologica Sinica,2000,18(1):63-67.［康安,朱筱敏,王贵文,等.古水深曲线在测井资料层序地层分析中的应用［J］.沉积学报,2000,18(1):63-67.］ 

［22］Liu Zhen,Shao Xinjun,Jin Bo,et al.Co-effect of depth and burial time on the evolution of porosity for classic rocks during the stage of compaction［J］.Geoscience,2007,21(1):125-132.［刘震,邵新军,金博,等.压实过程中埋深和时间对碎屑岩孔隙度演化的共同影响［J］.现代地质,2007,21(1):125-132.］

［23］Embley R W.New evidence for occurrence of debris flow deposits in the deep sea［J］.Geology,1976,4(1):371-374.

［24］Guo Zhanqian,Wang Xianbin.Volcanic activity,formation and evolution of sedimentary basin［J］.Earth Science：Journal of China University of Geosciences,1998,23(1):59-64.［郭占谦,王先彬.火山活动与沉积盆地的形成和演化［J］.地球科学,1998,23(1):59-64.］
[1] 王俊,高银山,王洪君,王新星,鲍志东,张红静. 基于正演模拟的水下分流复合河道内单一河道划分[J]. 天然气地球科学, 2018, 29(9): 1310-1322.
[2] 白雪峰, 梁江平, 张文婧, 付丽, 彭建亮, 薛涛, 杨立伟, 刘继莹. 松辽盆地北部深层天然气地质条件、资源潜力及勘探方向[J]. 天然气地球科学, 2018, 29(10): 1443-1454.
[3] 王颖, 邓守伟, 范晶, 邹晓品, 杨静. 松辽盆地南部重点断陷天然气地质条件、资源潜力及勘探方向[J]. 天然气地球科学, 2018, 29(10): 1455-1464.
[4] 周翔，舒萍，于士泉，陈曦. 松辽盆地徐深9区块营一段火山岩气藏储层特征及综合评价[J]. 天然气地球科学, 2018, 29(1): 62-72.
[5] 任丽华，代俊杰，林承焰，曹铮. 松辽盆地扶新隆起带南部青山口组超压特征及油气地质意义[J]. 天然气地球科学, 2017, 28(7): 1020-1030.
[6] 黄玉龙，刘春生，张晶晶，高有峰. 松辽盆地白垩系火山岩气藏有效储层特征及成因[J]. 天然气地球科学, 2017, 28(3): 420-428.
[7] 梁建设，田兵，王琪，马晓峰，牟炜卫. 深水沉积理论研究现状、存在问题及发展趋势[J]. 天然气地球科学, 2017, 28(10): 1488-1496.
[8] 袁静，王尉，朱建峰，陈杏霞，赵鸿皓. 松辽盆地长岭断陷龙凤山次凹下白垩统营城组物源与沉积相研究[J]. 天然气地球科学, 2017, 28(1): 93-105.
[9] 陈彬滔，潘树新，方乐华，张庆石，李成刚，梁苏娟. 松辽盆地齐家—古龙凹陷青山口组泥页岩层段储层特征[J]. 天然气地球科学, 2016, 27(2): 298-308.
[10] 陈瑞银，王汇彤，陈建平，刘玉莹. 实验方法评价松辽盆地烃源岩的生排烃效率[J]. 天然气地球科学, 2015, 26(5): 915-921.
[11] 詹路锋，邓宏文，郑文波. 叠前波形反演技术在深水扇储层预测中的应用[J]. 天然气地球科学, 2015, 26(4): 711-717.
[12] 刘超，印长海，卢双舫. 变系数ΔLgR烃源岩测井评价技术关键参数厘定方法及应用[J]. 天然气地球科学, 2015, 26(10): 1925-1931.
[13] 王卓卓,施立志，张永生. 松辽盆地北部大庆长垣浅层气成藏特征分析[J]. 天然气地球科学, 2014, 25(9): 1350-1357.
[14] 王民,孙业峰，王文广，王岩，石蕾. 松辽盆地北部徐家围子断陷深层烃源岩生气特征及天然气资源潜力[J]. 天然气地球科学, 2014, 25(7): 1011-1018.
[15] 施立志，王卓卓，张永生. 松辽盆地齐家地区高台子油层致密油分布及地质特征[J]. 天然气地球科学, 2014, 25(12): 1943-1950.
Viewed
Full text


Abstract

Cited
  Shared   
  Discussed   
No Suggested Reading articles found!