用介形类优势分异度恢复古湖盆的水深——以山东东营凹陷古近系沙河街组沙三段湖盆为例

英文篇名：Water depth of palaeo-lacustrine basin recovered by dominance diversity of Ostracoda:An example from sedimentary period of the Member of Shahejie Formation of Paleogene in Dongying Sag,Shandong Province
中文刊名：古地理学报
英文刊名：Journal of Palaeogeography
作者：李守军 ; 郑德顺 ; 姜在兴 ; 胡斌 ; 王金香 ; 焦叶红
英文作者：Li Shoujun 1 ; 2 Zheng Deshun Jiang Zaixing 4 Hu Bin 5 Wang Jinxiang 1 ; 2 Jiao Yehong 1 ; 2 1 Geoinformation Science and Engineering College ; Shandong University of Science and Technology ; Qingdao 266510 ; Shandong 2 Shandong Research Center of Engineering & Technology of Petroleum Exploration and Development ; Qingdao 266510 ; Shandong Institute of Earth Resource and Information ; China University of Petroleum (East China) ; Dongying 257061 ; Shandong 4 Department of Energy Geology ; China University of Geosciences ; Beijing 10008 5 Department of Resource and Environment ; Jiaozuo Institute of Technology ; Jiaozuo 454100 ; Henan
中文关键词：水深 ; 古湖盆 ; 介形类 ; 优势分异度 ; 古近系 ; 东营凹陷
英文关键词：water depth ; palaeo-lacustrine basin ; Ostracoda ; dominance diversity ; Paleogene ; Dongying Sag
出版日期：2005-09-10
机构：山东科技大学地球信息科学与工程学院,中国石油大学(华东)地球资源与信息学院,中国地质大学能源地质系,焦作工学院资源与环境工程系,山东科技大学地球信息科学与工程学院,山东科技大学地球信息科学与工程学院山东青岛266510,山东省油气勘探开发工程技术研究中心,山东青岛266510 ,山东东营257061 ,北京100083 ,河南焦作454100 ,山东青岛266510,山东省油气勘探开发工程技术研究中心,山东青岛266510 ,山东青岛266510,山东省油气勘探开发工程技术研究中心,山东青岛266510
年：2005
期：03
出版单位：古地理学报

摘要

从定量古生态学的角度出发,利用生态学和古生态学的资料,对介形类的优势分异度H(s)和古湖泊水深D的关系进行了相关性拟合,并得出了两者之间的关系。利用古近系东营三角洲地震资料和沉积学资料验证了这种对应关系的可信性,因此得出利用定量计算的介形类优势分异度值可以较准确地确定古水深。以东营凹陷古近系沙三段沉积时期为例,恢复了3个亚段沉积时期的古水深,并做出了平面等值线图。结果表明,东营凹陷的古水深由大到小依次为中亚段沉积时期、下亚段沉积时期和上亚段沉积时期。湖泊古水深的定量恢复,对于含油气盆地的油气生、储、盖研究具有重要的意义。
From the viewpoint of quantitative palaeoecology,the relationship is simulated and established between dominance diversity of Ostracoda (Hs) and water depth of palaeo-lacustrine basin (D) using ecology and palaeoecology data.The relationship is proved creditable based on seismic and sedimentary data of the Paleogene of Dongying Delta,thus the water depth can be accurately calculated using quantitatively calculated dominance diversity.Taking the sedimentary period of the Member of Shahejie Formation of Paleogene in Dongying Sag as an example,paleo-water depths of the submember sedimentary periods were recovered and the planar isoline maps were made.Results show that palaeo-water depths decreased from middle submember sedimentary period to lower submember sedimentary period and to upper submember sedimentary period in Dongying Sag.Quantitative recovery of water depth of palaeo-lacustrine basin is very important in the study of source rocks,reservoirs and caprocks of pertroliferous basin.

引文

拜尔斯著.1977.冯增昭等译.1987.停滞缺氧盆地中的生物相模式——一个通用模式.见CookHE和EnosP编.1977.冯增昭等译.1987.深水碳酸盐环境.北京:地质出版社,1～16
    毕义泉.2002.山东尚南断块古近系东营组沉积相及其古地理.古地理学报,4(3):19～25
    胜利油田石油地质志编写组.1993.中国石油地质志(卷六),胜利油田分册.北京:石油工业出版社,32～46,104～135
    田海芹,马玉新,赵勇生,等.2000.东营凹陷尚南断块东营组沉积层序研究.古地理学报,2(2):37～45
    杨式溥.1993.古生态学——原理与方法.北京:地质出版社,151～156
    姚益民,梁鸿德,蔡治国,等.1994.中国油气区第三系(IV),渤海湾盆地油气区分册.北京:石油工业出版社,102～144
    郑德顺,李守军.2002.山东东营凹陷古近纪介形类优势分异度研究.古地理学报,4(2):64～70
    中国科学院兰州地质所,等.1979.青海湖综合考察报告.北京:科学出版社,1～270
    中国科学院南京地理与湖泊研究所,等.1989.云南断陷湖泊环境与沉积.北京:科学出版社,1～513
    中国科学院南京地理与湖泊研究所.1990.抚仙湖.北京:科学出版社,1～317
    ByersCW.1977.Biofaciespatternsineuxinicbasins:ageneralmodel.In:CookHE,EnosP(eds).1977.FengZengzhao(trans).1987.Deepwatercarbonateenvironments.SocietyofEconomicPaleontologistsandMineralogistsSpecialPublicationsNo.25.Tulsa,Oklahoma,USA,5～17
    BiYiquan.2002.SedimentaryfaciesandpalaeogeographyofDongyingFormationofPaleogeneofSouthShangdianFaultblockinShandongProvince.JournalofPalaeogeography,4(3):19～25(inChinesewithEnglishabstract)
    DoddJR,StantonJrRJ.1981.Paleoecology:ConceptsandApplications.JonWiley&SonsInc,NewYork,1～546
    EditorialCommitteeofPetroleumGeologyofShengliOilfield.1993.PetroleumGeologyofChina,Vol.6,ShengliOilfield.Beijing:PetroleumIndustryPress,32～46,104～135(inChinese)
    LanzhouInstituteofGeology,ChineseAcademyofSciences,etal.1979.ComprehensiveInvestigationReportofQinghaiLake.Beijing:SciencePress,1～270(inChinese)
    NanjingInstituteofGeographyandLimnology,ChineseAcademyofSciences,etal.1989.EnvironmentsandDepositsintheFaultBasinsofYunnanProvince.Beijing:SciencePress,1～513(inChinese)
    NanjingInstituteofGeographyandLimnology,ChineseAcademyofSciences.1990.FuxianLake.Beijing:SciencePress,1～317(inChinese)
    TianHaiqin,MaYuxin,ZhaoYongsheng,etal.2000.StudiesonthesequencestratigraphyoftheDongyingFormation,SouthShangdianFaultblockofDongyingSag.JournalofPalaeogeography,2(2):37～45(inChinesewithEnglishabstract)
    WangPinxian,ZhaoQuanhong.1985.OstracodadistributioninbottomsedimentsofEastChinaSea.In:MarineMicropaleontologyofChina.Beijing:ChinaOceanPress,70～92
    YangShipu.1993.Palaeoecology:PrinciplesandMethods.Beijing:GeologicalPublishingHouse,151～156(inChinese)
    YaoYimin,LiangHongde,CaiZhiguo,etal.1994.TertiaryinPetroliferousRegionsofChina,Vol.4:TheBohaiGulfBasin.Beijing:PetroleumIndustryPress,102～144(inChinese)
    ZhengDeshun,LiShoujun.2002.StudyonthedominancediversityofOstracodaofthePaleogeneinDongyingSagofShandong.JournalofPalaeogeography,4(2):64～70(inChinesewithEnglishabstract)