徐家围子断陷南部沙河子组层序地层格架及沉积特征SEQUENCE STRATIGRAPHIC FRAMEWORK AND SEDIMENTARY CHARACTERISTICS FOR SHAHEZI FORMATION IN SOUTH XUJIAWEIZI FAULT DEPRESSION
蔡来星,卢双舫,巩兴会,王海生,魏然
CAI Laixing,LU Shuangfang,GONG Xinghui,WANG Haisheng,WEI Ran
摘要(Abstract):
针对徐家围子断陷南部沙河子组层序地层格架划分不清、沉积特征不明的现状,综合利用岩心、测井及地震等资料,应用Vail层序地层学理论,开展了徐家围子断陷南部沙河子组层序划分研究,并结合构造活动背景、物源供给情况分析了层序格架内的沉积相类型和演化特征。研究认为:南部沙河子组划分为1个二级层序,进一步划分为4个三级层序,每个三级层序均具有二分结构,发育湖侵、湖退2个体系域;研究区主要发育扇三角洲相、辫状河三角洲相和湖泊相等沉积相类型,以三角洲前缘亚相中的水下分流河道为主力储层砂体;南部沙河子组可归结为断控斜坡背景和缓坡背景的2种沉积模式,具有格架控砂、继承演化、分源沉积、连片发育的沉积演化特征。
In the light of the unclear current conditions of the sequence stratigraphic framework division and sedimentary characteristics for Shahezi Formation in South Xujiaweizi Fault Depression,by comprehensively using the core,well logging,seismic data and so on,the sequence division of the formation is conducted with the help of Vail sequence stratigraphy theory,and in the meantime integrating with the documents of the tectonic settings and provenance supply,the types of the sedimentary facies and evolutionary characteristics within the sequence framework are analyzed.The studies show that South Shahezi Formation can be divided into one second-class sequences and furthermore it can be classified into four third-class sequences,and moreover each third-class sequence possesses dichotomy structure and develops lacustrine transgressive and regressive system tracts;the sedimentary facies types such as fan delta,braided river delta and lacustrine facies and so on are well developed in the study area;South Shahezi Formation can be summarized into two sedimentary modes;fault-controlled steep and gentle slope settings,and furthermore possess the following sedimentary evolution characteristics:framework controlled sand,successive evolution,separated-source sedimentation and contiguous distribution.
关键词(KeyWords):
层序地层格架;沉积演化模式;沙河子组;徐家围子断陷南部
sequence stratigraphic framework;sedimentary evolution mode;Shahezi Formation;South Xujiaweizi Fault Depression
基金项目(Foundation): 国家油气重大专项(2011ZX05007-001);; 中央高校基本科研业务费专项资金(24720132103A)资助
作者(Author):
蔡来星,卢双舫,巩兴会,王海生,魏然
CAI Laixing,LU Shuangfang,GONG Xinghui,WANG Haisheng,WEI Ran
参考文献(References):
- [1]Jiang Z X,Lu H B,Yu W Q,et al.Transformation of accommodation space of the Cretaceous Qingshankou Formation,the Songliao Basin,NE China[J].Basin Research,2005,17(4):569-580.
- [2]姜在兴.沉积体系及层序地层学研究现状及发展趋势[J].石油与天然气地质,2010,31(5):535-541.
- [3]吴因业,朱如凯,罗平,等.沉积学与层序地层学研究新进展——第18届国际沉积学大会综述[J].沉积学报,2011,29(1):199-206.
- [4]卜淘.松辽盆地北部断陷期层序地层特征[J].成都理工大学学报:自然科学版,1999,26(4):382-384.
- [5]平贵东.三肇凹陷葡萄花油层多边断层成因机制及控藏机理研究[D].大庆:东北石油大学,2011.
- [6]夏利.徐家围子沙河子组沉积体系与烃源岩预测[D].北京:中国地质大学,2009.
- [7]殷进垠,刘和甫,迟海江.松辽盆地徐家围子断陷构造演化[J].石油学报,2002,23(2):26-29.
- [8]李霞,范宜仁,杨立伟,等.测井曲线小波变换特性在层序地层划分中的应用[J].大庆石油地质与开发,2006,25(4):112-115.
- [9]周祺,郑荣才,李凤杰,等.测井曲线在陆相层序地层界面识别中的应用——以鄂尔多斯盆地榆林气田山西组2段为例[J].大庆石油地质与开发,2008,27(4):135-138.
- [10]张志坚.松辽盆地jE部泰康地区高台子油层四砂组沉积微相特征[J].大庆石油地质与开发,2005,24(3):11-13.
- [11]刘喜武,党毅敏,杨波.松辽盆地北部大庆长垣以东地区深层沉积特征[J].大庆石油地质与开发,1998,17(5):16-18.
- [12]刘秋宏,卢双舫,李军辉,等.海拉尔盆地呼和湖凹陷南屯组层序地层与沉积体系分析[J].沉积学报,2010,28(2):227-234.
- [13]万传彪,乔秀云,孔惠,等.黑龙江北安地区早白垩世孢粉组合[J].微体古生物学报,2002,19(1):83-90.
- [14]岳云雷,于兴河,李胜利,等.坳陷湖盆缓坡层序地层及沉积体系研究——以准噶尔盆地陆西地区为例[J].大庆石油地质与开发,2007,26(3):43-46.
- [15]廖远涛,王华,王家豪,等.黄骅坳陷中区古近系东营组沉积特征及有利勘探区带预测[J].古地理学报,2009,11(5):561-572.
- 层序地层格架
- 沉积演化模式
- 沙河子组
- 徐家围子断陷南部
sequence stratigraphic framework - sedimentary evolution mode
- Shahezi Formation
- South Xujiaweizi Fault Depression