金州断裂带北段深孔地应力测量及其活动性
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摘要
为查明辽东半岛金州地震活动断裂带现今地应力状态和活动状况,在该断裂带北段熊岳城东侧开展了随深度系统地取心钻探和水压致裂地应力测量工作,完成了600m钻探深度范围内地应力测量试验27段和水平最大主应力方向测试5段.钻探岩心初步揭示了地壳浅表层的岩体结构特征;随深度系统的地应力测量结果表明,3个主应力关系为SV>SH>Sh,垂直应力起主导作用,易于正断作用发生;现今最大水平主应力方向为56°~81°NE,反映NNE走向的金州断裂带北段现今活动具有右行走滑特征.地应力测量结果揭示的金州断裂带正断兼右行走滑特征与已有的该区域研究成果相吻合,为其现今活动性研究补充了新的动力学数据.
Haicheng earthquake occurred in the north segment of Jinzhou fracture belt which is the most important active tectonic structure controlling earthquakes in Liaodong Peninsula.In this study,data was collected from 27in-situ stress and 5directional testing sensors installed at varying intervals along the total depth of single 600 mborehole located inside a granite rich region in the north segment of Jinzhou fracture belt at the east part of Xiongyue city.Combined with in-situ stress data of SV>SH>Sh,core sampling of the structural features of shallow earth crust rock formations reveals that the vertical principal stress plays a leading role in normal fault activity. Moreover,measured maximum in-situ principal stress trends towards the northeast-east direction and reflects present tensile properties,with dextral activity,of the Jinzhou segment.The results confirm the previous relevant studies,enriching the dynamics data and facilitating the understanding of the active features of the north segment of the Jinzhou fracture belt.
Haicheng earthquake occurred in the north segment of Jinzhou fracture belt which is the most important active tectonic structure controlling earthquakes in Liaodong Peninsula.In this study,data was collected from 27in-situ stress and 5directional testing sensors installed at varying intervals along the total depth of single 600 mborehole located inside a granite rich region in the north segment of Jinzhou fracture belt at the east part of Xiongyue city.Combined with in-situ stress data of SV>SH>Sh,core sampling of the structural features of shallow earth crust rock formations reveals that the vertical principal stress plays a leading role in normal fault activity. Moreover,measured maximum in-situ principal stress trends towards the northeast-east direction and reflects present tensile properties,with dextral activity,of the Jinzhou segment.The results confirm the previous relevant studies,enriching the dynamics data and facilitating the understanding of the active features of the north segment of the Jinzhou fracture belt.
引文
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Chen,Q.C.,An,Q.M.,Sun,D.S.,et al.,2010.Current InSitu Stress State of Shanxi Basin and Analysis of Earthquake Risk.Acta Geoscientica Sinica,31(4):541-548(in Chinese with English abstract).
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Feng,C.J.,Chen,Q.C.,Tan,C.X.,et al.,2013.Analysison Current In-Situ Stress State in Northern Segment ofLongmenshan Fault Belt.Progress in Geophysics,28(3):1109-1121(in Chinese with English abstract).
Feng,C.J.,Chen,Q.C.,Wu,M.L.,et al.,2012.Analysis ofHydraulic Fracturing Stress Measurement Data—Discussion of Methods Frequently Used to Determine Instantaneous Shut-In Pressure.Rock and Soil Mechanics,33(7):2149-2159(in Chinese with English abstract).
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Tan,C.X.,Sun,Y.,Wang,L.J.,2003.Some Problems ofIn-Situ Crustal Stress Measurements.Journal of Geomechanics,9(3):275-280(in Chinese with English abstract).
Tan,C.X.,Wang,R.J.,Sun,Y.,et al.,2004.NumericalModeling Estimation of the‘Tectonic Stress Plane’(TSP)Beneath Topography with Quasi-U-Shaped Valleys.International Journal of Rock Mechanics andMining Sciences,41(2):303-310.doi:10.1016/S1365-1609(03)00096-0
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Wang,L.,1988.A Discussion on the Stability of the Regional Crust with Interpretation on Structures by RemoteSensing Images in Yingkou Area.Liaoning Geology,(4):360-368(in Chinese with English abstract).
Wang,L.J.,Pan,L.Z.,Liao,C.T.,et al.,1991.In-SituStress Measurement and Its Application in Engineering.Geological Publishing House,Beijing(in Chinese).
Wang,T.M.,Xiang,H.F.,Fang,Z.J.,et al.,1976.A Studyof the Geotectonic Background and Seismogenic Structures of Haicheng Earthquake.Scientia Geologica Sinica,(3):205-212(in Chinese with English abstract).
Wang,Z.G.,Liu,C.,Feng,X.,et al.,2009.EarthquakeSpace Distribution and Its Relationships with MainFaults,Deep Structure and Stress Field in NortheastChina.Global Geology,28(4):513-519(in Chinesewith English abstract).
Wu,M.D.,1997.The Features of Activities and Seismic atJinzhou-Chaoyang Fault Belt in Liaoning Province.World Geology,16(1):39-42,48(in Chinese withEnglish abstract).
Wu,M.L.,Zhang,C.S.,Liao,C.T.,et al.,2005.The Recent State of Stress in the Central Qinghai-Tibet Plateau According to In-Situ Stress Measurements.ChineseJournal of Geophysics,48(2):327-332(in Chinesewith English abstract).
Wu,M.L.,Zhang,Y.Q.,Liao,C.T.,et al.,2010.Preliminary Results of In-Situ Stress along the LongmenshanFault Zone after the Wenchuan Ms8.0Earthquake.ActaGeologica Sinica,84(9):1292-1299(in Chinese withEnglish abstract).
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Xia,H.K.,Zhang,X.Z.,1986.Landforms of the Coastal Area of the Liaodong Peninsula and Their RepresentativeNeotectonic Motion.Seismology and Geology,8(1):41-49(in Chinese with English abstract).
Xie,F.R.,Chen,Q.C.,Cui,X.F.,et al.,2003.Study ofCrustal Stress Environment in China.Geological Publishing House,Beijing(in Chinese).
Zhang,B.C.,1996.Pore Pressure,Fault Slip Criterion andInfluence of Reservoir Impounding.In:Su,K.Z.,Li,F.Q.,Zhang,B.C.,et al.,eds.,Integrated Research onthe Stress Field and Pore Pressure at the Gorges Site.Seismological Press,Beijing(in Chinese).
Zhang,P.,Qin,X.H.,Feng,C.J.,et al.,2013.In-SituStress Measurement of Deep Borehole in Shandong Segment of Tan-Lu Fracture Belt and Analysis of Its Activity.Rock and Soil Mechanics,34(8):2329-2335(inChinese with English abstract).
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Zoback,M.D.,Healy,J.H.,1992.In-Situ Stress Measurements to 3.5km Depth in the Cajon Pass Scientific Research Borehole:Implications for the Mechanics ofCrustal Faulting.Journal of Geophysical Research,97(B4):5039-5057.doi:10.1029/91JB02175
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陈群策,安其美,孙东生,等,2010.山西盆地现今地应力状态与地震危险性分析.地球学报,31(4):541-548.
邓起东,王挺梅,李建国,等,1976.关于海城地震震源模式的讨论.地质科学,(3):195-204.
丁国瑜,1982.中国内陆活动断裂基本特征的探讨.北京:地震出版社.
丰成君,陈群策,谭成轩,等,2013.龙门山断裂带东北段现今地应力环境研究.地球物理学进展,28(3):1109-1121.
丰成君,陈群策,吴满路,等,2012.水压致裂应力测量数据分析———对瞬时关闭压力PS的常用判读方法讨论.岩土力学,33(7):2149-2159.
顾浩鼎,陈云泰,高祥林,等,1976.1975年2月4日辽宁省海城地震的震源机制.地球物理学报,19(4):270-285.
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Byerlee,J.,1978.Friction of Rocks.Pure and Applied Geophysics,116(4-5):615-626.doi:10.1007/BF00876528
Chen,Q.C.,An,M.J.,Li,F.Q.,1998.Theoretical Discussion on 3D Hydraulic Fracturing In Situ Stress Measurement.Journal of Geomechanics,4(1):37-44(inChinese with English abstract).
Chen,Q.C.,An,Q.M.,Sun,D.S.,et al.,2010.Current InSitu Stress State of Shanxi Basin and Analysis of Earthquake Risk.Acta Geoscientica Sinica,31(4):541-548(in Chinese with English abstract).
Deng,Q.D.,Wang,T.M.,Li J.G.,et al.,1976.A Discussion on Source Model of Haicheng Earthquake.ScientiaGeologica Sinica,(3):195-204(in Chinese with English abstract).
Ding,G.Y.,1982.Discussion on Basic Characteristics of ActiveBelts in China.Seismological Press,Beijing(in Chinese).
Feng,C.J.,Chen,Q.C.,Tan,C.X.,et al.,2013.Analysison Current In-Situ Stress State in Northern Segment ofLongmenshan Fault Belt.Progress in Geophysics,28(3):1109-1121(in Chinese with English abstract).
Feng,C.J.,Chen,Q.C.,Wu,M.L.,et al.,2012.Analysis ofHydraulic Fracturing Stress Measurement Data—Discussion of Methods Frequently Used to Determine Instantaneous Shut-In Pressure.Rock and Soil Mechanics,33(7):2149-2159(in Chinese with English abstract).
Gu,H.D.,Chen,Y.T.,Gao,X.L.,et al.,1976.FocalMechanism of Haicheng,Liaoning Province,EarthquakeFebruary 4,1975.Acta Geophysica Sinica,19(4):270-285(in Chinese with English abstract).
Haimson,B.C.,Cornet,F.H.,2003.ISRM Suggested Methods for Rock Stress Estimation—Part 3:HydraulicFracturing(HF)and/or Hydraulic Testing of PreExisting Fractures(HTPF).International Journal ofRock Mechanics&Mining Sciences,40(7):1011-1020.doi:10.1016/j.ijrmms.2003.08.002
Hayashi,K.,Haimson B.C.,1991.Characteristics of Shut-InCurves in Hydraulic Fracturing Stress Measurementsand Determination of In Situ Minimum CompressiveStress.Journal of Geophysical Research,96(B11):18311-18321.doi:10.1029/91JB01867
Institute of Geomechanics,Chinese Academy of GeologicalSciences,Seismic Geological Brigade of China Earthquake Administration,1981.The Principle and Application of In-Situ Stress Measurement.Geological Publishing House,Beijing(in Chinese).
Li,J.H.,Yang,Z.,1987.Active Fault in Liaodong Peninsulaand the Tectonic Setting of the Jinzhou Earthquake ofMagnitude 6.North China Earthquake Sciences,5(2):81-86(in Chinese with English abstract).
Li,X.,Li,Y.,Jiang,H.,et al.,1998.Shock AbsorptionEffect of Jinzhou Fault.Seismological Research ofNortheast China,14(6):24-27(in Chinese with English abstract).
Liaoning Bureau of Geology and Mineral Resources,1989.Regional Geology of Liaoning Province.Geological Publishing House,Beijing(in Chinese).
Liaoning Earthquake Administration,1996.Liaoning Province Records,Earthquake Records.Liaoning Science andTechnology Press,Shenyang(in Chinese).
Sun,Y.,Tan,C.X.,Li,K.S.,et al.,1998.Quantitative Evaluation of Regional Crustal Stability.Geological Publishing House,Beijing(in Chinese).
Sun,Y.,Tan,C.X.,Miao,P.S.,et al.,2012.Seismogeologyand Earthquake Prediction.Geological PublishingHouse,Beijing(in Chinese).
Tan,C.X.,Shi,L.,Sun,W.F.,et al.,2004.Research onTectonic Stress Plane.Chinese Journal of Rock Mechanics and Engineering,23(23):3970-3978(in Chinese with English abstract).
Tan,C.X.,Sun,W.F.,Zhang,C.S.,et al.,2007.An Analysis on Variation of Crustal Stress States at the ShallowPart of Upper Crust in Deep-Cut Valley Region.Progress in Geophysics,22(4):1353-1359(in Chinesewith English abstract).
Tan,C.X.,Sun,Y.,Wang,L.J.,2003.Some Problems ofIn-Situ Crustal Stress Measurements.Journal of Geomechanics,9(3):275-280(in Chinese with English abstract).
Tan,C.X.,Wang,R.J.,Sun,Y.,et al.,2004.NumericalModeling Estimation of the‘Tectonic Stress Plane’(TSP)Beneath Topography with Quasi-U-Shaped Valleys.International Journal of Rock Mechanics andMining Sciences,41(2):303-310.doi:10.1016/S1365-1609(03)00096-0
Wan,B.,Li,Y.T.,Zheng,S.C.,2010.Determination ofSeismogenic Structure for the East of Pulandian M6.0Earthquake in 1861.Earthquake Research in China,26(3):304-313(in Chinese with English abstract).
Wang,L.,1988.A Discussion on the Stability of the Regional Crust with Interpretation on Structures by RemoteSensing Images in Yingkou Area.Liaoning Geology,(4):360-368(in Chinese with English abstract).
Wang,L.J.,Pan,L.Z.,Liao,C.T.,et al.,1991.In-SituStress Measurement and Its Application in Engineering.Geological Publishing House,Beijing(in Chinese).
Wang,T.M.,Xiang,H.F.,Fang,Z.J.,et al.,1976.A Studyof the Geotectonic Background and Seismogenic Structures of Haicheng Earthquake.Scientia Geologica Sinica,(3):205-212(in Chinese with English abstract).
Wang,Z.G.,Liu,C.,Feng,X.,et al.,2009.EarthquakeSpace Distribution and Its Relationships with MainFaults,Deep Structure and Stress Field in NortheastChina.Global Geology,28(4):513-519(in Chinesewith English abstract).
Wu,M.D.,1997.The Features of Activities and Seismic atJinzhou-Chaoyang Fault Belt in Liaoning Province.World Geology,16(1):39-42,48(in Chinese withEnglish abstract).
Wu,M.L.,Zhang,C.S.,Liao,C.T.,et al.,2005.The Recent State of Stress in the Central Qinghai-Tibet Plateau According to In-Situ Stress Measurements.ChineseJournal of Geophysics,48(2):327-332(in Chinesewith English abstract).
Wu,M.L.,Zhang,Y.Q.,Liao,C.T.,et al.,2010.Preliminary Results of In-Situ Stress along the LongmenshanFault Zone after the Wenchuan Ms8.0Earthquake.ActaGeologica Sinica,84(9):1292-1299(in Chinese withEnglish abstract).
Xia,H.K.,1991.The Feature of Jinzhou Active Fault Zoneand Its Relation with Seismicity.North China Earthquake Sciences,9(2):21-28(in Chinese with Englishabstract).
Xia,H.K.,Zhang,X.Z.,1986.Landforms of the Coastal Area of the Liaodong Peninsula and Their RepresentativeNeotectonic Motion.Seismology and Geology,8(1):41-49(in Chinese with English abstract).
Xie,F.R.,Chen,Q.C.,Cui,X.F.,et al.,2003.Study ofCrustal Stress Environment in China.Geological Publishing House,Beijing(in Chinese).
Zhang,B.C.,1996.Pore Pressure,Fault Slip Criterion andInfluence of Reservoir Impounding.In:Su,K.Z.,Li,F.Q.,Zhang,B.C.,et al.,eds.,Integrated Research onthe Stress Field and Pore Pressure at the Gorges Site.Seismological Press,Beijing(in Chinese).
Zhang,P.,Qin,X.H.,Feng,C.J.,et al.,2013.In-SituStress Measurement of Deep Borehole in Shandong Segment of Tan-Lu Fracture Belt and Analysis of Its Activity.Rock and Soil Mechanics,34(8):2329-2335(inChinese with English abstract).
Zhao,W.F.,1989.The Feature of Seismic Structural inLiaoning Province.Northeastern Seismological Research,5(3):15-24(in Chinese with English abstract).
Zoback,M.D.,Healy,J.H.,1992.In-Situ Stress Measurements to 3.5km Depth in the Cajon Pass Scientific Research Borehole:Implications for the Mechanics ofCrustal Faulting.Journal of Geophysical Research,97(B4):5039-5057.doi:10.1029/91JB02175
陈群策,安美建,李方全,1998.水压致裂法三维地应力测量的理论探讨.地质力学学报,4(1):37-44.
陈群策,安其美,孙东生,等,2010.山西盆地现今地应力状态与地震危险性分析.地球学报,31(4):541-548.
邓起东,王挺梅,李建国,等,1976.关于海城地震震源模式的讨论.地质科学,(3):195-204.
丁国瑜,1982.中国内陆活动断裂基本特征的探讨.北京:地震出版社.
丰成君,陈群策,谭成轩,等,2013.龙门山断裂带东北段现今地应力环境研究.地球物理学进展,28(3):1109-1121.
丰成君,陈群策,吴满路,等,2012.水压致裂应力测量数据分析———对瞬时关闭压力PS的常用判读方法讨论.岩土力学,33(7):2149-2159.
顾浩鼎,陈云泰,高祥林,等,1976.1975年2月4日辽宁省海城地震的震源机制.地球物理学报,19(4):270-285.
中国地质科学院地质力学研究所,国家地震局地震地质大队,1981.地应力测量的原理和应用.北京:地质出版社.
李建华,杨喆,1987.辽东半岛活动断裂和金州6级地震的构造背景.华北地震科学,5(2):81-86.
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