台湾车笼埔断层深井钻探计划(TCDP)概述
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摘要
台湾车笼埔断层深井钻探计划(TCDP)是台湾车笼埔断层上进行的科学钻探工程。该计划于2004年开始实施,拟通过深达2 000 M的钻探,获取台湾1999年集集MW7.7地震深部断层带的岩芯样本和流体观测资料,并通过一系列的深井探测和观测研究,分析车笼埔断裂产生剧烈错动的原因。本文介绍了台湾车笼埔断层深井钻探计划(TCDP)的基本情况,论述了TCDP项目的科学假设、工作计划、合作项目以及近期的进展。全面了解TCDP相关内容,对我国大陆进行地震研究和深井钻探工作具有重要借鉴意义。
The Taiwan Chelongpu-fault scientific drilling program(TCDP) was put in practice in 2004.This program would drill a 2000 m deep hole on the Chelongpu-fault.The significance of this program is to obtain a physical sample of the fault where large displacements occurred during Taiwan Chi-Chi earthquake in 1999,to measure the physical properties and mechanical behavior of the rocks and fluid of the fault zone and to thoroughly understand the state of stress that exists in these rocks following such a large slip event.This paper has introduced the basic condition of TCDP,and elaborates on related contents,such as scientific supposition,work plan,cooperation project and recent progress.To realize the TCDP is useful to us for future seismic investigation and fault drilling.
The Taiwan Chelongpu-fault scientific drilling program(TCDP) was put in practice in 2004.This program would drill a 2000 m deep hole on the Chelongpu-fault.The significance of this program is to obtain a physical sample of the fault where large displacements occurred during Taiwan Chi-Chi earthquake in 1999,to measure the physical properties and mechanical behavior of the rocks and fluid of the fault zone and to thoroughly understand the state of stress that exists in these rocks following such a large slip event.This paper has introduced the basic condition of TCDP,and elaborates on related contents,such as scientific supposition,work plan,cooperation project and recent progress.To realize the TCDP is useful to us for future seismic investigation and fault drilling.
引文
[1]KANAMORIH AND T H HEATON.M ICSOSCPOIC AND M ACROSCOP IC PHYSICS OF EARTHQUAKES.GEOCOMP LEXITY AND THEPHYSICS OF EARTHQUAKES,2000,147-163
[2]B RODSKY E AND H KANAMORI.E LASTOHYDRODYNAM IC LUBRICATION OF FAU LTS.J.GEOPHYS.RES,2001,106:16 357-16 374
[3]M A K F,J MORI,S J LEE,ET AL.SPATIAL AND TEMPORAL D ISTRIBUTION OF SLIP FOR THE 1999 CH I-CH I,TAIWAN,EARTHQUAKE.BU LL.SE ISMO.SOC.AM,2001,91:1 069-1 087
[4]ZOBACK M D,M L ZOBACK,V S MOUNT,ET AL.NEW EVIDENCE ON THE STATE OF STRESS OF THE SAN ANDREAS FAU LTSYSTEM.SC IENCE,1981,238:1105-1 111
[5]H ICKM AN S.STRESS IN THE L ITHOSPHERE AND THE STRENGTH OF ACTIVE FAU LTS,U.S.NAT.REP.INT.UN ION GEOD.GEOPHYS.1987—1990,REV.GEOPHYS,1991,29:759-775
[6]SUPPE J,J H W ITTKE.ABNORM AL PORE-F LU ID PRESSURES IN RELATION TO STRATIGRAPHY AND STRUTURE IN THE ACTIVEFOLD-AND-THRUST BELT OF NORTH-WESTERN TAIWAN.PEROLEUM GEOLOGY OF TAIWAN,1977(14):11-24
[7]DAVIS D,J SUPPE AND F A DAHLEN.M ECHAN ICS OF FOLD-AND-THRUST-BELTS AND ACCRETIONARYW EDGES.J.GEOPHYS.RES,1983,88:1 153-1 172
[8]BARR T D AND F A DAHLEN.CONSTRAINTS ON FRICTION AND STRESS IN THE TAIWAN FOLD-SND-THRUST BELT FROM HEATF LOW AND GEOCHRONOLOGY.GEOLOGY,1990,18:111-115
[9]BRUDY M,M D ZOBACK,K FUCHS,ET AL.ESTIMATION OF THE COMPLETE STRESS TENSOR TO 8 KM DEPTH IN THE KTBSCIENTIFIC DRILL HOLES-IMPLICATION FOR CRUSTAL STRENGTH.J.GEOPHYS.RES,1997,102:18453-18475
[10]WIPRUT D,M D ZOBACK.FAULT REACTIVATION AND FLUID FLOW ALONG A PREVIOUSLY DORMANT NORMAL FAULT IN THENORWEGIAN NORTH SEA.GEOLOGY,2000,28(7):595-598
[11]TANAKA H,B SHIBAZAKI,N SHIGEMATSU,ET AL.GROWTH OF PLASTIC SHEAR ZONE AND ITS DURATION INFERRED FROMTHEORETICAL CONSIDERATION AND OBSERVATION OF AN ANCIENT SHEAR ZONE IN THE GRANITE CRUST.EARTH PLANETS SPACE,2002,54:1207-1210
[12]TANAKA A,HITO.TEMPERATURE AT THE BASE OF THE SEISMOGENIC ZONE AND ITS RELATIONSHIP TO THE FOCAL DEPTH OFTHE WESTERN NAGANO PREFECTURE AREA.ZISIN,2002,SER.Ⅱ,55:1-19
[13]ROELOFFS E A,NMATSUMOTO.HYDRAULIC PROPERTIES AT THE GSJ HIRABAYASHI BOREHOLE IN THE NOJIMA FAULT FROM A-NALYSIS OF PUMP TEST AND TIME SERIES DATA,IN PROCEEDINGS OF THE INTERNATIONAL WORKSHOP ON THE NOJIMA FAULTCORE AND BOREHOLE DATA ANALYSIS(EDITED BY H.ITO,K.FUJIMOTO,H.TANAKA AND D.LOCKNER),GSJ INTERIMREPORT.,EQ/00/1,USGS OPEN FILE REPORT,00-129,173-177,2000
[14]ABERCROMBIE R.EARTHQUAKE SOURCE SCALING RELATIONSHIPS FROM-1 TO 5MLUSING SEISMOGRAMS RECORDED AT2.5 KM DEPTH.J.GEOPHY.RES,1995,100:24015-24036
[15]ITO S,HITO,W L ELLSWORTH,ET AL.THE SLOWINITIAL PHASE OF EARTHQUAKES IN WESTERN NAGANO,CENTRAL JAPAN.SEISMOGENIC PROCESS MONTIORING,2002,117:103-117
[16]LI Y G,J E VIDALE,S MDAY,ET AL.CHARACTERIZATION OF RUPTURE ZONES OF THE HECTOR MINE AND LANDERS,CALI-FORNIA,EARTHQUAKE USING FAULT-ZONE TRAPPED WAVE.EOS.SUPPLEMENT,2000,DEC.81.F858
[17]TADOKORO K,MANDO,KNISHIGAMI.INDUEED EARTHQUAKES ACCOMPANYING THE WATER INJECTION EXPERIMENT AT THENOJIMA FAULT ZONE,JAPAN;SEISMICITY AND ITS MIGRATION.J.GEOPHY.RES.,2000,105:6089-6104
[18]ANDO M,N OSHIMAN,TSHIMAMOTO,ET AL.NOJIMA FAULT-ZONE PROBE.SPECIAL ISSUE OF ISLAND ARCSVOLUME 10.SEPTEMBER/DECEMBER.2001
[19]ITO H,K FUJIMOTO,HTANAKA,ET AL.PROCEEDINGS OF THE INTERNATIONAL WORKSHOP OF THE NOJIMA FAULT CORE ANDBOREHOLE DATA ANALYSIS.PP.1-289,GSJ INTERIM REPORT NO.EQ/00/1;USGS,OPEN-FILE REPORT00-129,1999
①蔡义本.台湾科技报道文献.2004。
[2]B RODSKY E AND H KANAMORI.E LASTOHYDRODYNAM IC LUBRICATION OF FAU LTS.J.GEOPHYS.RES,2001,106:16 357-16 374
[3]M A K F,J MORI,S J LEE,ET AL.SPATIAL AND TEMPORAL D ISTRIBUTION OF SLIP FOR THE 1999 CH I-CH I,TAIWAN,EARTHQUAKE.BU LL.SE ISMO.SOC.AM,2001,91:1 069-1 087
[4]ZOBACK M D,M L ZOBACK,V S MOUNT,ET AL.NEW EVIDENCE ON THE STATE OF STRESS OF THE SAN ANDREAS FAU LTSYSTEM.SC IENCE,1981,238:1105-1 111
[5]H ICKM AN S.STRESS IN THE L ITHOSPHERE AND THE STRENGTH OF ACTIVE FAU LTS,U.S.NAT.REP.INT.UN ION GEOD.GEOPHYS.1987—1990,REV.GEOPHYS,1991,29:759-775
[6]SUPPE J,J H W ITTKE.ABNORM AL PORE-F LU ID PRESSURES IN RELATION TO STRATIGRAPHY AND STRUTURE IN THE ACTIVEFOLD-AND-THRUST BELT OF NORTH-WESTERN TAIWAN.PEROLEUM GEOLOGY OF TAIWAN,1977(14):11-24
[7]DAVIS D,J SUPPE AND F A DAHLEN.M ECHAN ICS OF FOLD-AND-THRUST-BELTS AND ACCRETIONARYW EDGES.J.GEOPHYS.RES,1983,88:1 153-1 172
[8]BARR T D AND F A DAHLEN.CONSTRAINTS ON FRICTION AND STRESS IN THE TAIWAN FOLD-SND-THRUST BELT FROM HEATF LOW AND GEOCHRONOLOGY.GEOLOGY,1990,18:111-115
[9]BRUDY M,M D ZOBACK,K FUCHS,ET AL.ESTIMATION OF THE COMPLETE STRESS TENSOR TO 8 KM DEPTH IN THE KTBSCIENTIFIC DRILL HOLES-IMPLICATION FOR CRUSTAL STRENGTH.J.GEOPHYS.RES,1997,102:18453-18475
[10]WIPRUT D,M D ZOBACK.FAULT REACTIVATION AND FLUID FLOW ALONG A PREVIOUSLY DORMANT NORMAL FAULT IN THENORWEGIAN NORTH SEA.GEOLOGY,2000,28(7):595-598
[11]TANAKA H,B SHIBAZAKI,N SHIGEMATSU,ET AL.GROWTH OF PLASTIC SHEAR ZONE AND ITS DURATION INFERRED FROMTHEORETICAL CONSIDERATION AND OBSERVATION OF AN ANCIENT SHEAR ZONE IN THE GRANITE CRUST.EARTH PLANETS SPACE,2002,54:1207-1210
[12]TANAKA A,HITO.TEMPERATURE AT THE BASE OF THE SEISMOGENIC ZONE AND ITS RELATIONSHIP TO THE FOCAL DEPTH OFTHE WESTERN NAGANO PREFECTURE AREA.ZISIN,2002,SER.Ⅱ,55:1-19
[13]ROELOFFS E A,NMATSUMOTO.HYDRAULIC PROPERTIES AT THE GSJ HIRABAYASHI BOREHOLE IN THE NOJIMA FAULT FROM A-NALYSIS OF PUMP TEST AND TIME SERIES DATA,IN PROCEEDINGS OF THE INTERNATIONAL WORKSHOP ON THE NOJIMA FAULTCORE AND BOREHOLE DATA ANALYSIS(EDITED BY H.ITO,K.FUJIMOTO,H.TANAKA AND D.LOCKNER),GSJ INTERIMREPORT.,EQ/00/1,USGS OPEN FILE REPORT,00-129,173-177,2000
[14]ABERCROMBIE R.EARTHQUAKE SOURCE SCALING RELATIONSHIPS FROM-1 TO 5MLUSING SEISMOGRAMS RECORDED AT2.5 KM DEPTH.J.GEOPHY.RES,1995,100:24015-24036
[15]ITO S,HITO,W L ELLSWORTH,ET AL.THE SLOWINITIAL PHASE OF EARTHQUAKES IN WESTERN NAGANO,CENTRAL JAPAN.SEISMOGENIC PROCESS MONTIORING,2002,117:103-117
[16]LI Y G,J E VIDALE,S MDAY,ET AL.CHARACTERIZATION OF RUPTURE ZONES OF THE HECTOR MINE AND LANDERS,CALI-FORNIA,EARTHQUAKE USING FAULT-ZONE TRAPPED WAVE.EOS.SUPPLEMENT,2000,DEC.81.F858
[17]TADOKORO K,MANDO,KNISHIGAMI.INDUEED EARTHQUAKES ACCOMPANYING THE WATER INJECTION EXPERIMENT AT THENOJIMA FAULT ZONE,JAPAN;SEISMICITY AND ITS MIGRATION.J.GEOPHY.RES.,2000,105:6089-6104
[18]ANDO M,N OSHIMAN,TSHIMAMOTO,ET AL.NOJIMA FAULT-ZONE PROBE.SPECIAL ISSUE OF ISLAND ARCSVOLUME 10.SEPTEMBER/DECEMBER.2001
[19]ITO H,K FUJIMOTO,HTANAKA,ET AL.PROCEEDINGS OF THE INTERNATIONAL WORKSHOP OF THE NOJIMA FAULT CORE ANDBOREHOLE DATA ANALYSIS.PP.1-289,GSJ INTERIM REPORT NO.EQ/00/1;USGS,OPEN-FILE REPORT00-129,1999
①蔡义本.台湾科技报道文献.2004。
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