地球物理方法在城市活断层探测中的应用研究——以哈尔滨城市活断层探测项目为例
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摘要
从活动断裂的研究和进展出发,通过追溯国内外活动断裂研究发展历史,结合国际当前活动断裂研究的方法与趋势,认为地球物理方法是城市活断层探测的重要方法之一。文中重点介绍了在城市地震活断层探测中用到的地球物理方法的类型和主要特点,特别是在区域探查与初步鉴定阶段、详细探测与精确定位阶段、孕震构造探测阶段可能涉及到的各种地球物理探测方法、适用范围及所能解决的主要问题。同时,结合哈尔滨城市活断层探测项目实例,证明地球物理方法在城市活断层探测工作中甚为有效。
Reviewing the research of the active faults at home and abroad and combining the method of the present research on the active fault abroad,the paper proposes that the geophysical method is one of the most important methods.In this paper,it introduces various kinds of possible geophysical methods for seismic active fault exploration and their main features.It also discusses the scope of application of related geophysical methods and the major problems that they can solve in the different periods of active fault exploration,such as regional survey or preliminary investigation,detailed exploration or precise location and so on.Meanwhile,the discussion proves that the geophysical method has a good effect on urban active fault detection through the example of active fault detection in Harbin city.
Reviewing the research of the active faults at home and abroad and combining the method of the present research on the active fault abroad,the paper proposes that the geophysical method is one of the most important methods.In this paper,it introduces various kinds of possible geophysical methods for seismic active fault exploration and their main features.It also discusses the scope of application of related geophysical methods and the major problems that they can solve in the different periods of active fault exploration,such as regional survey or preliminary investigation,detailed exploration or precise location and so on.Meanwhile,the discussion proves that the geophysical method has a good effect on urban active fault detection through the example of active fault detection in Harbin city.
引文
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[16]石波,邱学林,田洪琴.哈尔滨市地震场地的划分[J].城市勘测,2000,(1):18~23.
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[20]白登海,王立凤,孙洁等.2002.福州八一水库-尚干断裂的高密度电法和瞬变电磁法实验探测[J].地震地质,24(4):557~564.
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[22]刘保金,张先康,方盛明,等.城市活断层探测的高分辨率浅层地震数据采集技术[J].地震地质,2002,24(4):524~532.
[23]刘启元.大陆岩石圈的宽频带流动地震台阵研究[A].见:刘若新.现今地球动力学及其应用[C].北京:地震出版社,1994.
[24]陆基孟.地震勘探原理[M].北京:石油大学出版社,1993.
[25]潘纪顺,刘保金,朱金芳,等.城市活断层高分辨率地震勘探震源对比试验研究[J].地震地质,2002,24(4):533~541.
[26]杨金山,张立忱,欧阳兆国,等.高密度电法在近场区断层探测中的应用[J].东北地震研究,2007,23(4):47~52.
[27]赵成斌,刘保金,姬继发,等.综合物探方法在地质灾害调查中的应用研究[J].物探与化探,2001,25(6):464~468.
[28]赵殿栋,郑泽继,吕公河,等.高分辨率地震勘探采集技术[J].石油地球物理勘探,2001,36(3):263~271.
[29]詹艳,赵国泽,梁竞阁,等.2001.PROTEM-37瞬变电磁测深系统及应用实例[J].地震地质,2001,23(2):26~270.
[30]曹令敏.应用浅层地震勘探划分地下软土结构[J].工程地球物理学报,2007,4(3):251~255.
[2]Calibers G.1977,Burghinoli,Effect of desiccatedcrust on the short-termstability of trenches in softclays,A Proc International Symposiumon Geotech-nical Aspects of Soft Clays,Bangkok,5 6 July1977,P437 451.Pub Bangkok:Asian Institute ofTechnology.
[3]Mohamed S,El-Genk and August W,Crone berg,1979,On the thermal stability of a frozen crust inforced flow on an insulated finite wall InternationalJournal of Heat and Mass Transfer,Volume 22,Is-sue 12,December 1979,Pages 1719~1723
[4]Hong ye.The North China Basin:An example of aCenozoic rifted inttraplate basin[J].Tectonics,1985,4(2).
[5]Wan Tianfeng,1984,Recent tectonic stress field,active faults and geothermal fields(hot-Watertype)in China,J.Vocanal.Geotherm.Res.22
[6]Jamison W R,Sprang J H.Use of calcite twin la-mellae to infer differential stress[J].Geol.Soc.A-mer Bull.1976,87(6)
[7]Molnar P.Cenozoic tectonics of Asia,effects of acontinental collision Science,1975,189.
[8]Baker B H.Continental rifting:progress and out-look,Eos.Vol.62 Slemmons D.B.et al.Defini-tions of Active Faults,pulished by US.Army En-gendering Waterways experi ment Station,Soil andPavement Laboratory.p.BOX631,1977.
[9]杨华,李金铭,桂峰.电阻率层析成像方法技术近年发展概况[J].球物理学进展,1998,13(4):90~96.
[10]刘志新,岳建华,刘仰光.矿井物探技术在突水预测中的应用[J].工程地球物理学报,2007,4(3):251~255.
[11]姚征,顾汉明,段洪友.提高泌阳凹陷深层系地震资料多次波压制效果的举措[J].工程地球物理学报,2006,3(5):370~374.
[12]陈培善,1973.极值理论在中长期地震预报中的应用[J].地球物理进展,1973,16(2):41~43.
[13]朱德兵.工程地球物理方法技术研究现状综述[J].地球物理学进展,2002,17(1):41~451
[14]邱增强,刘志新.2005,无线电波透视法在探测隐伏导含水构造中的应用[J].工程地球物理学报,2005,2(3):185~190.
[15]陈立春,梁辉,冉勇康等.2006.哈尔滨市主要断裂未来地震危险性评价[J].地震地质,2006,28(4):675~689.
[16]石波,邱学林,田洪琴.哈尔滨市地震场地的划分[J].城市勘测,2000,(1):18~23.
[17]汪素云.中国及邻近区现在构造应力场的数学模拟[J].地球物理学报,1980,23(1):24~29.
[18]陈庆宣.运用地质力学方法研究区域地壳稳定性[M].地质力学文集,第9集:1989:112~131.
[19]方盛明,张先康,刘保金,等.探测大城市活断层的地球物理方法[J].地震地质,2002,24(4):606~613.
[20]白登海,王立凤,孙洁等.2002.福州八一水库-尚干断裂的高密度电法和瞬变电磁法实验探测[J].地震地质,24(4):557~564.
[21]陈乐寿,王光锷.大地电磁测深法[M].北京:地质出版社,1990.
[22]刘保金,张先康,方盛明,等.城市活断层探测的高分辨率浅层地震数据采集技术[J].地震地质,2002,24(4):524~532.
[23]刘启元.大陆岩石圈的宽频带流动地震台阵研究[A].见:刘若新.现今地球动力学及其应用[C].北京:地震出版社,1994.
[24]陆基孟.地震勘探原理[M].北京:石油大学出版社,1993.
[25]潘纪顺,刘保金,朱金芳,等.城市活断层高分辨率地震勘探震源对比试验研究[J].地震地质,2002,24(4):533~541.
[26]杨金山,张立忱,欧阳兆国,等.高密度电法在近场区断层探测中的应用[J].东北地震研究,2007,23(4):47~52.
[27]赵成斌,刘保金,姬继发,等.综合物探方法在地质灾害调查中的应用研究[J].物探与化探,2001,25(6):464~468.
[28]赵殿栋,郑泽继,吕公河,等.高分辨率地震勘探采集技术[J].石油地球物理勘探,2001,36(3):263~271.
[29]詹艳,赵国泽,梁竞阁,等.2001.PROTEM-37瞬变电磁测深系统及应用实例[J].地震地质,2001,23(2):26~270.
[30]曹令敏.应用浅层地震勘探划分地下软土结构[J].工程地球物理学报,2007,4(3):251~255.
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