东海深井地球物理长期观测仪器设置与观测研究
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摘要
<正>东海深井地球物理长期观测是我国开展深井地震学观测研究的第一步,其目的是为了排除地面干扰,取得高信噪比、高分辨率和高精度的地球物理观测资料.美国圣安德列斯断层项目组开展的深井综合地球物理观测研究项目在4 000m深井的不同深度处设置了多种观测仪器(Chavarria et al,2003),进行震源过程及地震预报等研究(Schleicher et al,2009;Tembe et al,2009;Jeppson,Tobin,2015).日本已建
引文
涂毅敏,陈运泰.2002.德国大陆超深钻井注水诱发地震的精确定位[J].地震学报,24(6):587-598.Tu Y M,Chen Y T.2002.The accurate location of the injection-induced microearthquakes in German continental deep drilling program[J].Acta Seismologica Sinica,24(6):587-598(in Chinese).
徐纪人,杨文采,赵志新,程振炎.2003.苏鲁大别造山带岩石圈三维P波速度结构特征[J].地质学报,77(4):577-582.Xu J R,Yang W C,Zhao Z X,Chen Z Y.2003.Three-dimensional velocity structures of the Sulu-Dabie orogen belt[J].Acta Geologica Sinica,77(4):577-582(in Chinese).
徐纪人,赵志新.2004.苏鲁造山带区域地壳山根结构特征[J].岩石学报,20(1):149-156.Xu J R,Zhao Z X.2004.Regional structure characteristics of crustal root of mountain beneath the Sulu orogenic belt[J].Acta Petrologica Sinica,20(1):149-156(in Chinese).
徐纪人,赵志新.2009.深井地球物理观测的最新进展与中国大陆科学钻探长期观测[J].地球物理学进展,24(4):1176-1182.Xu J R,Zhao Z X.2009.Recent advance of borehole geophysical observation and Chinese continental scientific drilling long-term observatory at depth[J].Progress in Geophysics,24(4):1176-1182(in Chinese).
徐纪人,高锦曦,赵志新,皮金云,曾祥芝,周云好,傅德荣.2012.江苏东海5000米深井地球物理长期观测的最新进展[J].国际地震动态,(6):129.Xu J R,Gao J X,Zhao Z X,Pi J Y,Zeng X Z,Zhou Y H,Fu D R.2012.New advance for borehole geophysical longterm observation of 5000mdepth in Donghai,Jiangsu[J].Recent Developments in Word Seismology,(6):129(in Chinese).
徐纪人,高锦曦,赵志新,皮金云,曾祥芝,周云好,傅德荣,曲明.2013.中国大陆科学钻探5000米深井地球物理长期观测最新进展[C]∥中国地球物理2013—第十分会场论文集.北京:中国地球物理学会:348.Xu J R,Gao J X,Zhao Z X,Pi J Y,Zeng X Z,Zhou Y H,Fu D R,Qu M.2013.New observation progress for 5000m depth borehole geophysical long-term observatory of Chinese continental scientific drilling[C]∥The Tenth Breakout of Chinese Geophysical Collection in 2003.Beijing:Chinese Geophysical Society:348(in Chinese).
徐纪人,赵志新,曾祥芝.2015.深井地球物理观测与东海深井长期观测的最新进展[J].国际地震动态,(9):108.Xu J R,Zhao Z X,Zeng X Z.2015.New advance for borehole geophysical observation and the borehole long-term observation in Donghai[J].Recent Developments in Word Seismology,(9):108(in Chinese).
石井紘.2010.応力連続観測と今後の地震予知研究:ボアホール応力連続観測計器の開発による今後の展開[J].地震ジャーナル,50(1):73-77.Ishii H.2010.Continual stress observation and earthquake prediction research:Prospect based on the development of borehole stress observation instrument[J].Earthquake Journal,50(1):73-77(in Japanese).
Chavarria J A,Malin P,Catchings R D,Shalev E.2003.A look inside the San Andreas Fault at Parkfield through vertical seismic profiling[J].Science,302(5651):1746-1748.
Fujimoto K,Ueda A,Ohtani T,Takahashi M,Ito H,Tanaka H,Boullier A M.2007.Borehole water and hydrologic model around the Nojima fault,SW Japan[J].Tectonophysics,443(3/4):174-182.
Ikali M J,Kameda J,Saffer D M,Kopf A J.2015.Strength characteristics of Japan Trench borehole samples in the highslip region of the 2011Tohoku-Oki earthquake[J].Earth Planet Sci Lett,412:35-41.
Jeppson T N,Tobin H J.2015.San Andreas Fault Zone velocity structure at SAFOD at core,log,and seismic scales[J].J Geophys Res,120(7):4983-4997.
Ma K F,Lin Y Y,Lee S J,Mori J,Brodsky E E.2012.Isotropic events observed with a borehole array in the Chelungpu fault zone,Taiwan[J].Science,337(6093):459-463.
Schleicher A M,Tourscher S N,van der Pluijm B A,Warr L N.2009.Constraints on mineralization,fluid-rock interaction,and mass transfer during faulting at 2-3km depth from the SAFOD drill hole[J].J Geophys Res,114(B4):B04202.
Tembe S,Lockner D,Wong T F.2009.Constraints on the stress state of the San Andreas Fault with analysis based on core and cuttings from San Andreas Fault Observatory at Depth(SAFOD)drilling phases 1and 2[J].J Geophys Res,114(B11):B11401.
Zhao Z,Zhao Z X,Xu J R.2012.Velocity structure heterogeneity and tectonic motion in and around the Tan-Lu fault of China[J].J Asian Earth Sci,57:6-14.
徐纪人,杨文采,赵志新,程振炎.2003.苏鲁大别造山带岩石圈三维P波速度结构特征[J].地质学报,77(4):577-582.Xu J R,Yang W C,Zhao Z X,Chen Z Y.2003.Three-dimensional velocity structures of the Sulu-Dabie orogen belt[J].Acta Geologica Sinica,77(4):577-582(in Chinese).
徐纪人,赵志新.2004.苏鲁造山带区域地壳山根结构特征[J].岩石学报,20(1):149-156.Xu J R,Zhao Z X.2004.Regional structure characteristics of crustal root of mountain beneath the Sulu orogenic belt[J].Acta Petrologica Sinica,20(1):149-156(in Chinese).
徐纪人,赵志新.2009.深井地球物理观测的最新进展与中国大陆科学钻探长期观测[J].地球物理学进展,24(4):1176-1182.Xu J R,Zhao Z X.2009.Recent advance of borehole geophysical observation and Chinese continental scientific drilling long-term observatory at depth[J].Progress in Geophysics,24(4):1176-1182(in Chinese).
徐纪人,高锦曦,赵志新,皮金云,曾祥芝,周云好,傅德荣.2012.江苏东海5000米深井地球物理长期观测的最新进展[J].国际地震动态,(6):129.Xu J R,Gao J X,Zhao Z X,Pi J Y,Zeng X Z,Zhou Y H,Fu D R.2012.New advance for borehole geophysical longterm observation of 5000mdepth in Donghai,Jiangsu[J].Recent Developments in Word Seismology,(6):129(in Chinese).
徐纪人,高锦曦,赵志新,皮金云,曾祥芝,周云好,傅德荣,曲明.2013.中国大陆科学钻探5000米深井地球物理长期观测最新进展[C]∥中国地球物理2013—第十分会场论文集.北京:中国地球物理学会:348.Xu J R,Gao J X,Zhao Z X,Pi J Y,Zeng X Z,Zhou Y H,Fu D R,Qu M.2013.New observation progress for 5000m depth borehole geophysical long-term observatory of Chinese continental scientific drilling[C]∥The Tenth Breakout of Chinese Geophysical Collection in 2003.Beijing:Chinese Geophysical Society:348(in Chinese).
徐纪人,赵志新,曾祥芝.2015.深井地球物理观测与东海深井长期观测的最新进展[J].国际地震动态,(9):108.Xu J R,Zhao Z X,Zeng X Z.2015.New advance for borehole geophysical observation and the borehole long-term observation in Donghai[J].Recent Developments in Word Seismology,(9):108(in Chinese).
石井紘.2010.応力連続観測と今後の地震予知研究:ボアホール応力連続観測計器の開発による今後の展開[J].地震ジャーナル,50(1):73-77.Ishii H.2010.Continual stress observation and earthquake prediction research:Prospect based on the development of borehole stress observation instrument[J].Earthquake Journal,50(1):73-77(in Japanese).
Chavarria J A,Malin P,Catchings R D,Shalev E.2003.A look inside the San Andreas Fault at Parkfield through vertical seismic profiling[J].Science,302(5651):1746-1748.
Fujimoto K,Ueda A,Ohtani T,Takahashi M,Ito H,Tanaka H,Boullier A M.2007.Borehole water and hydrologic model around the Nojima fault,SW Japan[J].Tectonophysics,443(3/4):174-182.
Ikali M J,Kameda J,Saffer D M,Kopf A J.2015.Strength characteristics of Japan Trench borehole samples in the highslip region of the 2011Tohoku-Oki earthquake[J].Earth Planet Sci Lett,412:35-41.
Jeppson T N,Tobin H J.2015.San Andreas Fault Zone velocity structure at SAFOD at core,log,and seismic scales[J].J Geophys Res,120(7):4983-4997.
Ma K F,Lin Y Y,Lee S J,Mori J,Brodsky E E.2012.Isotropic events observed with a borehole array in the Chelungpu fault zone,Taiwan[J].Science,337(6093):459-463.
Schleicher A M,Tourscher S N,van der Pluijm B A,Warr L N.2009.Constraints on mineralization,fluid-rock interaction,and mass transfer during faulting at 2-3km depth from the SAFOD drill hole[J].J Geophys Res,114(B4):B04202.
Tembe S,Lockner D,Wong T F.2009.Constraints on the stress state of the San Andreas Fault with analysis based on core and cuttings from San Andreas Fault Observatory at Depth(SAFOD)drilling phases 1and 2[J].J Geophys Res,114(B11):B11401.
Zhao Z,Zhao Z X,Xu J R.2012.Velocity structure heterogeneity and tectonic motion in and around the Tan-Lu fault of China[J].J Asian Earth Sci,57:6-14.
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