引文
[1]Zheng Xiufen,Ouyang Biao,Zhang Dongning,et al.Technicalsystem construction of data backup centre for China seismographnetwork and the data support to researches on the Wenchuan earth-quake[J].Chinese Journal of Geophysics,2009,52(5):1 412-1 417.[郑秀芬,欧阳飚,张东宁,等.“国家数字测震台网数据备份中心”技术系统建设及其对汶川大地震研究的数据支撑[J].地球物理学报,2009,52(5):1 412-1 417.]
[2]Guo Mengqiu,Fu Liyun.Review of methods for studying sourcezone stress changes from seismic data[J].Progress in Geophysics,2008,23(2):375-383.[郭梦秋,符力耘.利用地震观测资料预测震源区应力变化研究进展综述[J].地球物理学进展,2008,23(2):375-383.]
[3]Aggarwal Y P,Sykes L R,Armbruster J,et al.Premonitory chan-ges in seismic velocities and prediction of earthquakes[J].Nature,1973,241:101-104.
[4]Niu Fenglin,Silver Paul G,Daley Thomas M,et al.Preseismicvelocity changes observed from active source monitoring at theParkfield SAFOD drill site[J].Nature,2008,454:204-208.
[5]Birch F.The velocity of compressional waves in rocks to 10 kilo-bars,Part 1[J].Journal of Geophysical Research,1960,65:1 083-1 102.
[6]Birch F.The velocity of compressional waves in rocks to 10 kilo-bars,Part 2[J].Journal of Geophysical Research,1961,66:2 199-2 224.
[7]Nur A.Effects of stress on velocity anisotropy in rocks with cracks[J].Journal of Geophysical Research,1971,76:2 022-2 034.
[8]Simmons G.Velocity of shear waves in rocks to10 kilobars1[J].Journal of Geophysical Research,1964,69:1 123-1 130.
[9]Lumley D E.Time-lapse seismic reservoir monitoring[J].Geo-physics,2001,66(1):50-53.
[10]Song X D,Richards P G.Seismological evidence for differentialrotation of the Earth's inner core[J].Nature,1996,382:221-224.
[11]Shapiro N M,Campillo M,Stehly L,et al.High-resolution sur-face-wave tomography from Ambient seismic noise[J].Science,2005,307:1 615-1 618.
[12]Sens-Schnfelder C,Wegler U.Passive image interferometry andseasonal variations of seismic velocities at merapi volcano,Indo-nesia[J].Geophysical Research Letter,2006,33:L21302,doi:10.1029/2006GL027797.
[13]Chen Yong,Wang Baoshan,Ge Hongkui,et al.Proposed oftransmitted seismic stations[J].Advances in Earth Science,2007,22(5):441-446.[陈颙,王宝善,葛洪魁,等.建立地震发射台的建议[J].地球科学进展,2007,22(5):441-446.]
[14]Furumoto M,Yuko Ichimori,Nobunhiko Hayashi,et al.Seismicwave velocity changes and stress build-up in the crust of the Kan-to-Tokai region[J].Geophysical Research Letter,2001,28(19):3 737-3 740.
[15]YukutakeH,NakajimaT,Doi K.In situ measurementsof elasticwave velocity in a mine,and the effects of water and stress ontheir variation[J].Tectonophysics,1988,149:165-175.
[16]Sano O,Mizuta Y,Murakami T,et al.Sound velocity as ameasure of small stress change[C]∥Sugawara K,Obara Y,eds.Rock Stress:Proceedings of the International Symposium onRock Stress.Kumamoto:A A Balkema,Brookfield,Vt.,1997:241-246.
[17]Yamamura K,Sano O,Utada H,et al.Long-term observation ofin situ seismic velocity and attenuation[J].Journal of GeophysicalResearch,2003,108(B6):2 317.
[18]Silver PG,DaleyTM,Niu F,et al.Activesourcemonitoringofcross-well seismic traveltime for stress-induced changes[J].Bul-letin Seismological Society of America,2007,97:281-293.
[19]Li Yijin,Xin Wei,WangBaoshan,et al.Implementation of highprecision measurement of seismic velocity change using high sam-ple rate data-acquisition system[J].Seismological and Geomag-netic Observation and Research,2011,in press.[李宜晋,辛维,王宝善,等.利用高采样率数采实现地震波速变化高精度测量[J].地震地磁观测与研究,2011,待刊.]
[20]Baeten G,Ziolkowski A.The Vibroseis Source[M].Oxford:Elsevier,1990.
[21]Yamaoka K,Kunitomo T,Miyakawa K,et al.A trial for monito-ring temporal vaiation of seismic velocity using and ACROSS sys-tem[J].The Island Arc,2001,10:336-347.
[22]Ikuta R,YamaokaK,MiyakawaK,et al.Continuousmonitoringof propagation velocity of seismic wave using ACROSS[J].Geo-physical Research Letters,2002,29(13):1 627.
[23]Wang Hongti,Zhuang Cantao,Xue Bing,et al.Precisely andactively seismic monitoring[J].Chinese Journal of Geophysical,2009,52(7):1 805-1 815.[王洪体,庄灿涛,薛兵,等.精密主动地震监测[J].地球物理学报,2009,52(7):1 808-1 815.]
[24]Yang Wei,Ge Hongkui,Wang Baoshan,et al.Velocity changesobserved by the precisely controlled active source fro the MianzhuMs5.6 earthquake[J].Chinese Journal of Geophysical,2010,53(5):1 149-1 157.[杨微,葛洪魁,王宝善,等.由精密控制人工震源观测到的绵竹5.6级地震前后波速变化[J].地球物理学报,2010,53(5):1 149-1 157.]
[25]Alekseev A S,Chichinin I S,Korneev V A.Powerful low-fre-quency vibrators for active seismology[J].Bulletin SeismologicalSociety of America,2005,95:1-17.
[26]Wang Baoshan,Sun Daoyuan,Li Shengjie,et al.The effect ofheterogeneity on rock's ultrasonic attenuation and its correction[J].Earthquake Research in China,2001,17(1):1-7.[王宝善,孙道远,李生杰,等.岩石非均匀性对超声衰减的影响及其修正[J].中国地震,2001,17(1):1-7.]
[27]De Fazio T L,Aki K,Alba J.Solid earth tide and observedchange in the in situ seismic velocity[J].Journal of GeophysicalResearch,1973,78(8):1 319-1 322.
[28]Reasenberg P,Aki K.A precise,continuous measurement ofseismic velocity for monitoring in situ stress[J].Journal of Geo-physical Research,1974,79:399-406.
[29]Li Y G,Vidale J E,Oglesby D D,et al.Multiple-fault ruptureof the M7.1 Hector Mine California,earthquake from fault zonetrapped waves[J].Journal of Geophysical Research,2003,108(B3):2165,doi:10.1029/2001JB001456.
[30]Grêt A A,Snieder R,Zbay U.Monitoring in situ stress changesin a mining environment with coda wave interferometry[J].Geo-physical Journal International,2006,167(2):504-508.
[31]Wang Baoshan,Zhu Ping,Chen Yong,et al.Continuous sub-surface velocity measurement with coda wave interferometry[J].Journal of Geophysical Research,2008,113:B12313,doi:10.1029/2007JB005023.
[32]Wang Weitao,Wang Baoshan,Ge Hongkui,et al.Using activesource to monitor velocity variation in shallow sediment caused bythe Wenchuan earthquake[J].Earthquake Research in China,2009,25(3):223-233.[王伟涛,王宝善,葛洪魁,等.利用主动震源检测汶川地震余震引起的浅层波速变化[J].中国地震,2009,25(3):223-233.]
[33]Wang Baoshan,Yang Wei,Yuan Songyong,et al.An experi-mental study on the excitation of large volume airgun in small vol-ume water body[J].Journal of Geophysics and Engineering,2010,7:388-394.
[34]Okaya D,Henrys S,Stem T.Double-side onshore-offshore seis-mic imaging of a plate boundary:“Super-gathers”across southisland,New Zealand[J].Tectonophysics,2002,255:247-263.
[35]Qiu Xuelin,Chen Yong,Zhu Rixiang,et al.The application oflarge volume airgun sources to the onshore-offshore seismic sur-veys:Implication from the experimental results in South ChinaSea[J].Chinese Science Bulletin,2007,52(4):463-469.[丘学林,陈颙,朱日祥,等.大容量气枪震源在海陆联测中的应用:南海北部试验结果分析[J].科学通报,2007,52(4):463-469.]
[36]Leary P C,Malin P E,Phinny R A,et al.Systematic monitoringof millisecond travel time variations near Palmdale,California[J].Journal of Geophysical Research,1979,84:659-666.
[37]LearyPC,Malin PE.Millisecond accuratemonitoringof seismictravel times over 13-and 18-kilometer baselines[J].Journal ofGeophysical Research,1982,87:6 919-6 930.
[38]Chen Yong,Zhang Xiankang,Qiu Xuelin,et al.A new way togenerate seismic waves for continental crustal exploration[J].Chinese Science Bulletin,2007,52(11):1 317-1 321.[陈颙,张先康,丘学林,等.陆地人工激发地震波的一种新方法[J].科学通报,2007,52(11):1 317-1 321.]
[39]Lin Jianmin,Wang Baoshan,Ge Hongkui,et al.Study on largevolume airgun source characteristics and seismic phase analysis[J].Chinese Journal of Gophysics,2008,51(1):206-212.[林建民,王宝善,葛洪魁,等.大容量气枪震源特征及深部介质中传播的震相分析[J].地球物理学报,2008,51(1):206-212.]
[40]Lin Jianmin,Wang Baoshan,Ge Hongkui,et al.Characters oflarge volume airgun source excitation[J].Chinese Journal of Go-physics,2010,53(2):342-349.[林建民,王宝善,葛洪魁,等.大容量气枪震源子波激发特性分析[J].地球物理学报,2010,53(2):342-349.]
[41]Quazi A.An overview on the time delay estimate in active andpassive systems for target localization[J].IEEE Transaltions A-coustics,Speech and Signal Processing,1981,29(3):527-533.
[42]Carter G C.Coherence and time delay estimation[J].Proceed-ings of the IEEE,1987,75(2):236-255.
[43]Snieder R.The theory of coda wave interferometry[J].Pure andApplied Geophysics,2006,163:455-473.
[44]Zhang Wei,Dai Hengchang,Li Xiangyang,et al.Shear wavegenerated by airguns in a reservoir and its splitting[J].Seismolo-gy and Geology,2009,31(1):22-33.[张尉,戴恒昌,李向阳,等.水库气枪震源产生的S波分裂[J].地震地质,2009,31(1):22-33.]