东营凹陷始新统红层古沉积环境恢复及其地质意义RECOVERY OF THE PALAEOSEDEMENTARY ENVIRONMENT IN EOCENE RED FORMATIONS AND ITS GEOLOGICAL SIGNEFICANCES FOR DONGYING SAG
李继岩,宋国奇,高永进,杨学君
LI Jiyan,SONG Guoqi,GAO Yongjin,YANG Xuejun
摘要(Abstract):
综合运用元素ICP-AES分析、地质录井等资料,结合古生物观察、镜下薄片观察及全岩矿物X衍射分析等手段,利用定性和定量相结合的方法,对东营凹陷始新统红层的古沉积环境进行了恢复。研究认为:红层沉积时期古气候干旱,孢粉以裸子植物为主,被子植物次之,大多为旱生的麻黄粉属和三肋麻黄粉;红层为陆上暴露环境中的氧化沉积物,古水介质的古盐度较高,为淡水一微咸水环境,水介质呈现弱碱性一碱性特征;古沉积环境对沉积相类型、成岩作用特征具有一定的控制作用,古气候和水介质氧化还原性决定沉积相类型及沉积体系的展布特征,形成了"冲积扇一洪水一漫湖一盐湖"过渡的沉积体系,水介质的古盐度和酸碱性控制了早期成岩作用,对埋藏成岩作用具有一定的影响,形成了大量早期碳酸盐胶结物,为后期的溶蚀作用奠定了物质基础。
Integrating ICP-AES element analysis,mud logging and other data,and moreover combining with the paleontologic and thin-section observations,full rock mineral X diffraction analysis and other means,the recovery of palaeosedimentary environment in Eocene red formations of Dongying Sag is conducted with the integration of qualitative and quantitative methods.The results show that during the period of red formation deposition,the sporopollens are mianly from the gymnosperms,the next is angiosperms,most of them are xeric and three-rib Ephedripites;red formations are the oxidation deposit in the exposed environment on land.The paleosalinity of the palaeo-aqueous media are rather high,the fresh and brackish water environments are determined,the media are characterized by alkalescence and alkalinity.The types of sedimentary facies and diagenesis features are controlled to a certain degree by the palaeosedimentary environment,the former and distribution characteristics of the depositional system are determined by the redox conditions of the palaeoclimate and water media,thus the transitional depositional system of " alluvial-fan-floods-diffuse lake-salt lake" is generated.The early diagenesis is controlled by the paleosalinity and pH of the media,and furthermore they have a certain impact on the burial diagenesis.In the end,a large number of early canbonate cements are formed,thus the material foundation for late dissolution is laid.
关键词(KeyWords):
东营凹陷;始新统;红层;古气候;古盐度;氧化还原性;酸碱性
Dongying Sag;Eocene;red formation;palaeoclimate;paleosalinity,redox ability;pH
基金项目(Foundation): 国家油气科技重大专项(2008ZX05051);; 中央高校基本科研业务费专项资金(11CX06004A)资助
作者(Author):
李继岩,宋国奇,高永进,杨学君
LI Jiyan,SONG Guoqi,GAO Yongjin,YANG Xuejun
参考文献(References):
- [1]刘宝珺,张锦泉.沉积成岩作用[M].北京:科学出版社,1992:6-92.
- [2]姜在兴.沉积学[M].北京:石油工业出版社,2003:5-65.
- [3]苗军.柴达木盆地第三纪湖盆古水介质研究[J].西安石油学院学报:自然科学版,2000,15(4):22-25.
- [4]李进龙,陈东敬.古盐度定量研究方法综述[J].油气地质与采收率,2003,10(5):1-4.
- [5]赵伦,赵澄林,袁选俊.酒东盆地营尔凹陷古湖泊水介质研究[J].西安石油学院学报:自然科学版,1998,13(5):6-11.
- [6]杨香华,孙永传,孙家振.泌阳凹陷下第三系的层序地层格架及其对边界断裂、古气候和物源的响应[J].地球科学:中国地质大学学报,1994,19(4):666-674.
- [7]渠永宏,万传彪,杜恩泽,等.海拉尔—塔木察格盆地地层划分对比及勘探意义[J].大庆石油地质与开发,2010,29(5):53-59.
- [8]Couch E L.Calculation of paleosalinites from boron and clay mineral data[J].AAPG Bull,1971,55:1829-1839.
- [9]Walker C T.Evaluation of boron as a paleosalinity indicator and its application to offshore prospects[J].AAPG Bull,1968,52:751-766.
- [10]王丽岩,孙跃斌,乔秀云,等.海拉尔盆地早白垩世孢粉古气候特征[J].大庆石油地质与开发,2008,27(5):38-42.
- [11]刘继莹.海拉尔盆地查干诺尔凹陷大磨拐河组孢粉组合及其地质意义[J].大庆石油地质与开发,2011,30(3):51-58.
- [12]Huntley B.Studying global change:the contribution of quaternary palynology[J].Paleogeography,Paleoclimatology,Paleoecology(Global Planetary Change Section),1990,82:53-61.
- [13]Webb R S,Anderson K H,Webb T.Pollen responsesurface estimates of late Quaternary changes in the moisture balance of the northeastern United States[J].Quaternary Research,1993,40:213-227.
- [14]王建伟,赵勇生,田海芹.东营—惠民凹陷孔店组层序地层学研究[J].石油大学学报:自然科学版,2001,25(6):1-5.
- [15]徐磊.东营凹陷沙四下—孔一段沉积特征研究[D].青岛:中国石油大学,2008.
- [16]操应长,王健,高水进,等.济阳坳陷东营凹陷古近系红层—膏盐层沉积特征及模式[J].古地理学报,2011,13(4):375-386.
- [17]陈春强.东营凹陷古近系层序格架内储层成岩作用研究[D].北京:中国地质大学,2006。
- [18]周瑶琪,周振柱,陈勇,等.东营凹陷民丰地区深部储层成岩环境变化研究[J].地学前缘,2011,18(2):268-276.
- [19]张善文,袁静,隋风贵,等.东营凹陷北部沙河街组四段源部储层多重成岩环境及演化模式[J].地质科学,2008,43(3):576-587.
- [20]邱隆伟,赵伟,刘魁元.碱性成岩作用及其在济阳坳陷的应用展望[J].油气地质与采收率,2007,14(2):10-16.
- [21]刘清俊,于炳松,贾丽云,等.塔里木盆地志留系柯坪塔格组砂岩储层成岩作用[J].大庆石油地质与开发,2012,31(2):18-25.
- [22]汪新光,张建光,魏忠元,等.伊通地堑鹿乡断陷储层成岩作用特征[J].大庆石油地质与开发,2009,28(2):29-32.