引文
[1]陈颙,朱日祥.设立“地下明灯研究计划”的建议[J].地球科学进展,2005,20(5):485-489.
[2]陈颙,周华伟,葛洪魁.华北地震台阵探测计划[J].大地测量与地球动力学,2005,25(4):1-5.
[3]陈颙,张尉,陈汉林,等.地震雷达[J].地球物理学进展,2006,21(1):1-5.
[4]陈颙,朱日祥.发展“地震雷达”的设想[M]//中国地球物理学会年刊.长春:吉林大学出版社,2005:10-11.
[5]Kulhanek.The structure and interpretation ofseismograms[M]//International Handbook ofEarthquake and Engineering Seismology.AcademicPress,2002:333-348.
[6]Jeffrey Park,Kent Anderson,Richard Aster,et al.Global seismograms network records the greatSumatra-Andaman Earthquake,EOS[J].Transactions,American Geophysical Union,2005,86(6):57,60-61.
[7]Ni S,Kanamori H,Helmberger D.Energy radiationfrom the Sumatra earthquake[J].Nature,2005,434:582.
[8]Alekseev A S,Chichinin I S,Korneev V A.Powerfullow-frequency vibrators for active seismology[J].BullSeismol Soc Am,2005,95:1-17.doi:10.1785/012003026.
[9]Baeten G,Ziolkowski A.The Vibroseis Source[M].Oxford:Elsevier,1990.
[10]Dekorp Research Group.Wide-angle vibroseis datafrom the western Rhenish Massif[J].Tectonophysics,1990,173:83-93.
[11]Yamaoka K,Kunitomo T,Miyakawa K,et al.A trialfor monitoring temporal variation of seismic velocityusing and ACROSS system[J].The Island Arc,2001,10:336-347.
[12]Ikuta R,Yamaoka K,Miyakawa K,et al.Continuousmonitoring of propagation velocity of seismic waveusing ACROSS[J].Geophys Res Lett,2002,29:doi:10.1029/2001GL013974.
[13]Dragoset W.Introduction to air guns and air-gunarrays[J].The Leading Edge,2000,19(8):892-987.
[14]Ronen S.Psi,pascal,bars,and decibels[J].TheLeading Edge,2002,21(1):60-62.
[15]Caldewll J,Dragoset W.A brief overview of seismicair-gun arrays[J].The Leading Edge,2000,19(8):898-902.
[16]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,已投稿.
[17]周宝华,刘威北.气枪震源的发展与使用分析(上)[J].物探装备,1998,8(1):1-6.
[18]周宝华,刘威北.气枪震源的发展与使用分析(下)[J].物探装备,1998,8(2):1-5.
[19]罗桂纯,王宝善,葛洪魁,等.气枪震源在地球深部结构探测中的应用研究进展[J].地球物理学进展,2006,21:400-407.
[20]Maurice G B.Pulse Coding in Seismology[M].Boston:International Human Resources DevelopmentCorporation,1982.
[21]Okaya D,Henrys S,Stem T.Double-side onshore-offshore seismic i maging of a plate boundary:“super-gathers”across South Island,New Zealand[J].Tectonophysics,2002,255:247-263.
[22]Nazareth J J,Clayton R W.Crustal structure of theBorderland-Continent Transition Zone of southernCalifornia adjacent to Los Angeles[J].J Geophys Res,2003,108(B8).2404,doi:10.1029/2001JB000223.
[23]van Avendonk HJ A,Holbrook WS,Okaya D,et al.Continental crust under compression:a seismicrefraction study of South Island Geophysical TransectI,South Island,New Zealand[J].J Geophys Res,2004,109.B06302,doi:10.1029/2003JB002790.
[24]McIntosh K,Nakamura Y,Wang T K,et al.Crustal-scale seismic profiles across Tai wan and the westernPhilippine Sea[J].Tectonophysics,2005,401:23-54.
[25]Melhuish A,Holbrook WS,Davey F,et al.Crustaland upper mantle seismic structure of the AustralianPlate,South Island,New Zealand[J].Tectonophysics,2005,395:113-135.
[26]Cheng W B,Wang C,Shyu C T,et al.Crustalstructure of the convergent plate-boundary zone,eastern Tai wan,assessed by seismic tomography[J].Geological Society of America,2002,358(special):163-177.
[27]Qiu X,Ye S,Wu S,et al.Crustal structure across theXisha Trough,northwestern South China Sea[J].Tectonophysics,2001,341:179-193.
[28]葛洪魁,林建民,王宝善,等.编码震源提高地震探测能力的野外实验研究[J].地球物理学报,2006,49(3):864-870.
[29]Reasenberg P,Aki K.A precise,continuousmeasurement of seismic velocity for monitoring in situstress[J].J Geophys Res,1974,79:399-406.
[30]Schaff D P,Richards P G.Repeating seismic events inChina[J].Science,2004,303:1 176-1 178.
[31]Yamamura K,Sano O,Utada H,et al.Long-termobservation of in situ seismic velocity and attenuation[J].J Geophys Res,2003,108.2317,doi:10.1029/2002JB002005.
[32]Silver P G,Daley T M,Niu F et al.Active sourcemonitoring of crosswell seismic travel ti me for stressinduced changes[J].Bull Seismol Soc Am,2007,inpress.
[33]Karageorgi E,Clymer R,McEvilly T V.Seismologicalstudies at Parkfield.Ⅱ:search for temporal variationsin wave propagation using vibroseis[J].Bull SeismolAm,1992,82:1 388-1 415.