国内外地震科学钻探与测井技术应用
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摘要
大地震发生后,在断裂带开展科学钻探是研究地震发震机理的快速反应和科学计划手段。测井技术是重要的井中地球物理探测方法。本文结合日本Nojima断层科学钻探、美国San Andreas科学深钻、台湾车笼埔钻探和中国汶川地震科学钻探研究成果,综述了国内外地震科学钻探计划实施和研究进展,对比和分析了测井技术在其中发挥的作用和取得的成果。最后,对地震科学钻探井中观测研究提出了建议,并展望了测井技术在地震科学钻探中的应用。
New information about large earthquakes can be acquired by drilling into the fault zone quickly following a large seismic event,which is important for the study on the seismic mechanism in the fault zones.Geophysical logging is an important geophysical means in boreholes.Recent progresses in scientific drilling programs were summarized,which included such as Janpan Nojima science drilling,U.S.San Andreas fault science drilling,the Taiwan Chelungpu drilling program,China Wenchuan Earthquake Scientific Drilling,and their applications of geophysical logging.The log analysis results and their roles were discussed and summarized.Finally,some advices about bore geophysical observation were proposed and the future demands of logging technology for earthquake scientific drilling were considered.
New information about large earthquakes can be acquired by drilling into the fault zone quickly following a large seismic event,which is important for the study on the seismic mechanism in the fault zones.Geophysical logging is an important geophysical means in boreholes.Recent progresses in scientific drilling programs were summarized,which included such as Janpan Nojima science drilling,U.S.San Andreas fault science drilling,the Taiwan Chelungpu drilling program,China Wenchuan Earthquake Scientific Drilling,and their applications of geophysical logging.The log analysis results and their roles were discussed and summarized.Finally,some advices about bore geophysical observation were proposed and the future demands of logging technology for earthquake scientific drilling were considered.
引文
[1]Emily E Brodsky,Jim Mori,Patrick M.Fulton,Drilling Into Faults Quickly After Earthquakes[J].Eos,2010,91(27):237-238.
[2]Zeev Reches,Hisao Ito.Scientific Drilling of Active Faults:Past and Future[M].2007,235-258.
[3]李斌凯,马海州,谭红兵.测井技术的应用及其在科学钻探研究中的意义[J].地球物理学进,2007,22(5):1 493-1 501.
[4]Volker Haak,Alan G.Jones,Introduction to Special Section:the KTB Deep Drill Hole[J].Journalof Geophysical Research,1997,102(8):175-177.
[5]李舟波,王祝文.德国大陆科学钻探计划的测井技术[J].国外地质勘探技术,1998,2:1-8.
[6]Pan Heping,Niu Yixiong,Wan Wenxian.CCSD Well Logging Engineering Program[J].Journal ofChina University of Geosciences,2002,1:91-94.
[7]牛一雄,潘和平,王文先,等.中国大陆科学钻探主孔(0~2 000m)地球物理测井[J].岩石学报,2004,20(1):165-178.
[8]Kentaro Omura,Ryuji Ikeda,Tatsuo Matsuda.Photographs of NIED Nojima fault drilling cores athirabayashi borehole—Technical note of the National Research Institute for Earth Science and Disas-ter Prevention[M].229,April,2002.
[9]Amy Day-Lewis,Mark Zoback,Stephen Hickman.An integrated study of a major plate-boundingfault at seismogenic depths of SAFOD[M].CLSI Workshop,Tokyo,October 3-4,2005.
[10]Boness L N,Zoback M D.Stress-induced seismic velocity anisotropy and physical properties in theSAFOD Pilot Hole in Parkfield[J].Geophys Res Lett,2003,31:L15S17.
[11]彭阜南,叶银灿.台湾9.21集集地震考察兼论强震发震断层[J].地震地质,2004,26(4):576-579.
[12]刘耀炜,陆斌,孙小龙.台湾车笼埔断层深井钻探计划(TCDP)概述[J].国际地震动态,2006,26(2):34-40.
[13]国土资源部中国地震局汶川地震断裂带科学钻探筹备组.“中国主要地震断裂带科学钻探计划”第一期工程——汶川地震断裂带科学钻探(WFSD)设计方案.
[14]Hiroaki Tsukahara,Ryuji Ikeda and Kiyohiko Yamamoto.In situ stress measurements in a boreholeclose to the Nojima fault[J].The island arc,2001,10:261-265.
[15]Masataka Ando.Geological and geophysical studies of the Nojima fault from drilling:an outline ofthe Nojima fault zone probe[J].The island arc,2001,10:206-214.
[16]Tsutomu Kiguchi,Hisaso Ito,Yasuto Kuwahara,et al.Estimating the permeability of the nojimafault zone by a hydrophone:vertical seismic profiling experiment[J].The island arc,2001,10:348-356.
[17]Kazuo Mizoguchi,Takehiro Hirose,Toshihiko Shimamoto,et al.Internal structure and permeabili-ty of the Nojima fault,southwest Japan[J].Journal of Structural Geology,2008,30:513-524.
[18]Zoback M D,Hickman S,Ellsworth W L.Scientific drilling into the San Andreas Fault[J].Eos,Trans AGU,2010,91(22):197-204.
[19]Mark Zoback,Stephen Hickman,William Ellsworth,and the SAFOD Science Team.Scientific drill-ing into the San Andreas Fault zone—An overview of SAFOD’s First Five Years[R].Scientific re-port,doi:10.2204/iodp.sd.11.02.2011.
[20]Hung-Yu Wu,Kuo-Fong Ma,Zoback M,et al.Stress orientations of Taiwan Chelungpu FaultDrilling Project(TCDP)hole as observed from geophysical logs[J].Geophys Res Lett,2007,25(1):33-40.
[21]Lin Weiren,Yeh Enchao,Hung Jihhao,et al.Localized rotation of principal stress around faultsand fractures determined from borehole breakouts in hole B of the Taiwan Chelungpu-fault DrillingProject(TCDP)[J].Tectonophysics,2010,482(1/4):82-91.
[22]胡时友,宋军,张伟,等.汶川地震断裂带科学钻探(WFSD)项目钻探和测井课题的组织实施与管理[J].探矿工程(岩土钻掘工程),2009,36(12):1-5.
[23]杨光,李海兵,张伟,等.四川龙门山安县—灌县断裂带的特征——以汶川地震断裂带科学钻探3号孔(WFSD-3)岩心为例[J].地质通报,2012,31(8):1 219-1 232.
[24]李朋武,崔军文,王连捷,等.中国大陆科学钻探主孔钻孔崩落与现场应力状态的确定[J].岩石学报,2005,21(2):421-426.
[25]邹长春,刘东明,聂昕,等.利用成像测井资料分析汶川地震断裂带科学钻探3号孔(WFSD-3)裂缝特征[J].现代地质,2012,26(6):1 150-1 153.
[26]聂昕,邹长春,肖昆,等.汶川地震断裂带科学钻探WFSD-1孔成像测井岩心空间归位[J].地球物理学进展,2012,27(1):75-82.
[27]汪集旸,胡圣标,程本合,等.中国大陆科学钻探先导孔地热测量[J].科学通报,2001,46(10):847-850.
[28]朱留方.交叉偶极子阵列声波测井资料在裂缝性储层评价中的应用[J].测井技术,2003,27(1):225-227.
[29]杨文采.大陆科学钻探与中国科学深钻工程[J].石油地球物理勘探,2002,37(2):196-200.
[30]Philippe Gaillot,Hideki Masago,Moe Kyaw Thu,et al.Core-Log-Seismic Integration-New Scien-tific and Technological Challenges[A].In scientific drilling and coring[C].Tokyo,Japan,October3-4,2005.
[2]Zeev Reches,Hisao Ito.Scientific Drilling of Active Faults:Past and Future[M].2007,235-258.
[3]李斌凯,马海州,谭红兵.测井技术的应用及其在科学钻探研究中的意义[J].地球物理学进,2007,22(5):1 493-1 501.
[4]Volker Haak,Alan G.Jones,Introduction to Special Section:the KTB Deep Drill Hole[J].Journalof Geophysical Research,1997,102(8):175-177.
[5]李舟波,王祝文.德国大陆科学钻探计划的测井技术[J].国外地质勘探技术,1998,2:1-8.
[6]Pan Heping,Niu Yixiong,Wan Wenxian.CCSD Well Logging Engineering Program[J].Journal ofChina University of Geosciences,2002,1:91-94.
[7]牛一雄,潘和平,王文先,等.中国大陆科学钻探主孔(0~2 000m)地球物理测井[J].岩石学报,2004,20(1):165-178.
[8]Kentaro Omura,Ryuji Ikeda,Tatsuo Matsuda.Photographs of NIED Nojima fault drilling cores athirabayashi borehole—Technical note of the National Research Institute for Earth Science and Disas-ter Prevention[M].229,April,2002.
[9]Amy Day-Lewis,Mark Zoback,Stephen Hickman.An integrated study of a major plate-boundingfault at seismogenic depths of SAFOD[M].CLSI Workshop,Tokyo,October 3-4,2005.
[10]Boness L N,Zoback M D.Stress-induced seismic velocity anisotropy and physical properties in theSAFOD Pilot Hole in Parkfield[J].Geophys Res Lett,2003,31:L15S17.
[11]彭阜南,叶银灿.台湾9.21集集地震考察兼论强震发震断层[J].地震地质,2004,26(4):576-579.
[12]刘耀炜,陆斌,孙小龙.台湾车笼埔断层深井钻探计划(TCDP)概述[J].国际地震动态,2006,26(2):34-40.
[13]国土资源部中国地震局汶川地震断裂带科学钻探筹备组.“中国主要地震断裂带科学钻探计划”第一期工程——汶川地震断裂带科学钻探(WFSD)设计方案.
[14]Hiroaki Tsukahara,Ryuji Ikeda and Kiyohiko Yamamoto.In situ stress measurements in a boreholeclose to the Nojima fault[J].The island arc,2001,10:261-265.
[15]Masataka Ando.Geological and geophysical studies of the Nojima fault from drilling:an outline ofthe Nojima fault zone probe[J].The island arc,2001,10:206-214.
[16]Tsutomu Kiguchi,Hisaso Ito,Yasuto Kuwahara,et al.Estimating the permeability of the nojimafault zone by a hydrophone:vertical seismic profiling experiment[J].The island arc,2001,10:348-356.
[17]Kazuo Mizoguchi,Takehiro Hirose,Toshihiko Shimamoto,et al.Internal structure and permeabili-ty of the Nojima fault,southwest Japan[J].Journal of Structural Geology,2008,30:513-524.
[18]Zoback M D,Hickman S,Ellsworth W L.Scientific drilling into the San Andreas Fault[J].Eos,Trans AGU,2010,91(22):197-204.
[19]Mark Zoback,Stephen Hickman,William Ellsworth,and the SAFOD Science Team.Scientific drill-ing into the San Andreas Fault zone—An overview of SAFOD’s First Five Years[R].Scientific re-port,doi:10.2204/iodp.sd.11.02.2011.
[20]Hung-Yu Wu,Kuo-Fong Ma,Zoback M,et al.Stress orientations of Taiwan Chelungpu FaultDrilling Project(TCDP)hole as observed from geophysical logs[J].Geophys Res Lett,2007,25(1):33-40.
[21]Lin Weiren,Yeh Enchao,Hung Jihhao,et al.Localized rotation of principal stress around faultsand fractures determined from borehole breakouts in hole B of the Taiwan Chelungpu-fault DrillingProject(TCDP)[J].Tectonophysics,2010,482(1/4):82-91.
[22]胡时友,宋军,张伟,等.汶川地震断裂带科学钻探(WFSD)项目钻探和测井课题的组织实施与管理[J].探矿工程(岩土钻掘工程),2009,36(12):1-5.
[23]杨光,李海兵,张伟,等.四川龙门山安县—灌县断裂带的特征——以汶川地震断裂带科学钻探3号孔(WFSD-3)岩心为例[J].地质通报,2012,31(8):1 219-1 232.
[24]李朋武,崔军文,王连捷,等.中国大陆科学钻探主孔钻孔崩落与现场应力状态的确定[J].岩石学报,2005,21(2):421-426.
[25]邹长春,刘东明,聂昕,等.利用成像测井资料分析汶川地震断裂带科学钻探3号孔(WFSD-3)裂缝特征[J].现代地质,2012,26(6):1 150-1 153.
[26]聂昕,邹长春,肖昆,等.汶川地震断裂带科学钻探WFSD-1孔成像测井岩心空间归位[J].地球物理学进展,2012,27(1):75-82.
[27]汪集旸,胡圣标,程本合,等.中国大陆科学钻探先导孔地热测量[J].科学通报,2001,46(10):847-850.
[28]朱留方.交叉偶极子阵列声波测井资料在裂缝性储层评价中的应用[J].测井技术,2003,27(1):225-227.
[29]杨文采.大陆科学钻探与中国科学深钻工程[J].石油地球物理勘探,2002,37(2):196-200.
[30]Philippe Gaillot,Hideki Masago,Moe Kyaw Thu,et al.Core-Log-Seismic Integration-New Scien-tific and Technological Challenges[A].In scientific drilling and coring[C].Tokyo,Japan,October3-4,2005.
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