测井和地震联合解释CCSD先导孔反射体
详细信息 本馆镜像全文    |  推荐本文 | | 获取馆网全文
摘要
利用声波、密度、自然伽玛等测井曲线资料、配合录井资料划分CCSD先导孔变质岩岩性,然后,用声波、密度计算波阻抗,与井旁VSP资料对比,分析CCSD先导孔孔区反射体.分析结果表明(1)岩性间波阻抗差异产生反射波,如榴辉岩与副片麻岩之间波阻抗差异;榴辉岩与超基性蛇纹岩之间的波阻抗差异等;(2)破碎特别是韧性剪切带产生反射波,而如果断层破碎带尺度很小(在1m以下),也不一定能产生强反射波.这些研究结果对标定地壳中的反射地震信号具有重要意义.
The main aim of this paper is to analyze reflectors in the pilot hole of CCSD (China Continental Scientific Drilling). The lithology of the metamorphite in the CCSD pilot hole can be identified by logging curves and geo-logging data. The wave impedance can be calculated by using acoustic (AC) and density log (DEN) curves. By comparing the acoustic wave impedance with the VSP (vertical seismic profile), the reflectors of the CCSD pilot hole have been analyzed. The results indicate that reflected waves are primarily produced by the wave impedance properties of the lithology (such as the wave impedance difference between eclogite and paragneiss or between eclogite and ultrabasic serpentinite, etc) and the fracture. The fractures are mainly the ductile shear zones. If the fracture thickness is less than 1m, reflectors cannot be produced. The study provides significant data concerning the interpretation of seismic reflection signals in the earth's crust.
引文
Feng,X.,Liu,C.,Yang,B.J.,etal.,2001.Theproducingmethodandtheapplicationofsyntheticseismogramofhighprecision.WorldGeology,20(4):389-395(inChinesewithEnglishabstract).
    Li,C.W.,Li,F.D.,Ren,H.J.,etal.,2002.IntroductionofscientificdrillingengineeringforChinacontinents.Pe-troleumDrillingTechniques,30(5):4-6(inChinesewithEnglishabstract).
    Pan,H.P.,Niu,Y.X.,Wang,W.X.,2002.CCSDwelllog-gingprogram.JournalofChinaUniversityofGeosci-ences,13(1):91-94.
    Pan,H.P.,Niu,Y.X.,Wang,W.X.,2004.Studyofpetrophys-icscharactersusinglogginginformationinpre-pilotholeⅡofCCSD.ChineseJournalofEngineeringGeophysics,1(1):10-16(inChinesewithEnglishabstract).
    Tang,Z.M.,Chai,Y.C.,Chen,S.Z.,etal.,2005.Deformationcharacteristicsofthegraniticgneissunitfromthe1113-1160mcoreofCCSDmainhole.GeologyinChina,32(2):265-274(inChinesewithEnglishabstract).
    Yang,W.C.,Chen,Z.Y.,Chen,G.J.,etal.,1999a.GeophysicalinvestigationsinnorthernSuluUHPMbelt,PartⅠ:Deepseismicreflection.ChineseJournalofGeophysics,42(1):41-50(inChinesewithEnglishabstract).
    Yang,W.C.,Fang,H.,Chen,Z.Y.,etal.,1999b.Geophysicalin-vestigationofnorthernSuluUHPMterraneingeophysicalinvestigationofnorthernSuluUHPMterraneineastChina(Ⅱ):Non-seismicmethods.ChineseJournalofGeophysics,42(4):508-517(inChinesewithEnglishabstract).
    Yang,W.C.,Zhang,C.H.,Zhu,G.M.,etal.,2002.Cali-brationofseismicreflectorsinChinesecontinentaldrill-ingarea.ChineseJournalofGeophysics,45(3):370-384(inChinesewithEnglishabstract).
    Zhang,W.H.,2002.JointapplicationofVSPandsoniclog-gingdatainlithologicinterpretation.GeophysicalPros-pectingforPetroleum,41(2):149-153(inChinesewithEnglishabstract).
    Zhang,Y.K.,1998.ContinentalscientificdrillingandlocationofthefirstsuperdeepdrillinginChina.GeologyinJiang-su,22(4):193-198(inChinesewithEnglishabstract).
    冯晅,刘财,杨宝俊,等,2001.高精度合成地震记录制作方法及应用.世界地质,20(4):389-395.
    李传武,李发东,任海军,等,2002.中国大陆科学钻探工程简介.石油钻探技术,30(5):4-6.
    潘和平,牛一雄,王文先,2004.测井资料提取中国大陆科学钻探PPⅡ孔岩石物性.工程地球物理学报,1(1):10-16.
    唐哲民,柴耀楚,陈世忠,等,2005.CCSD主孔1113~1600m花岗质片麻岩单元的变形构造特征.中国地质,32(2):265-274.
    杨文采,程振炎,陈国九,等,1999a.苏鲁超高压变质带北部地球物理调查(Ⅰ)——深反射地震.地球物理学报,42(1):41-50.
    杨文采,方慧,程振炎,等,1999b.苏鲁超高压变质带北部地球物理调查(Ⅱ)——非地震方法.地球物理学报,42(4):508-517.
    杨文采,张春贺,朱光明,2002.标定大陆科学钻探孔区地震反射体.地球物理学报,45(3):370-384.
    张卫红,2002.VSP和声波测井资料在岩性解释中的联合应用.石油物探,41(2):149-153.
    张永康,1998.大陆科学钻探与中国第一口科学钻选址.江苏地质,22(4):193-198.

版权所有:© 2023 中国地质图书馆 中国地质调查局地学文献中心