[1]A J Crone.Introduction to directions in paleoseismology,In:A J Crone and E M Omdahl eds.,Directions in Paleoseismology. U.S.Geol.Sruv. Open-File Rep.1987,87-673,pp1-6.
[2]Wallace.1981,Active Faults, Paleoseismology, and Earthquake hazard in the western United States,In:Simpson,In:Simpson D. W. and Review:Washington, D.C.,American Geophysical Union,Maurice Ewing Series 4,pp209-216.
[3]J McCalpin.Geologic Criteria for individual paleoseismic events in extensional environments.In:Simoson D W and Omdahl E M,eds. Directions in paleoseismology.U S Geol.Surv. Open-File Rep.1987,87-673,pp102-114.
[4]程绍平，杨桂枝编写.活断层研究中的槽探技术.地展地质译丛,1991.12(1).
[5]S Obcrrrieier. 1987，Iderstificatian and Geologic Characteristics of Earthquaka一iroduced Liquctaction Eeatures，In : A J Crone and E M Omdahl eds. Directions in paleoseismology. U. S. Geol. Surv. Ooen-File Rep. 87-673.pp173-177.
[6]J C Tinsley et al. 1985，Evaluating liquefaction Poiantial.ln:J I Ziong ed.Evaluating Earthquakes Hazrards in the Los Angeles Region:An Earth一science perspective,U. S. Geol.Surv. Prof. Paper 1360.pp263-316.
[7]N Ynaekura.Quaternary Tectonic Movennents in the Outcr arc of southwest Japan with Special Reference to Seismic Crustal Deformations,Bull.Deo. Geog.Univ. Tokyo:1975,7,pp19-71.
[8]G Plafker. 1987，Agplicaiion of marine一terrace data to paleaseismic studies, In:A J Crone and E M Omdahl eds.,Directions in paleoseismiolgy,U.S.Geol.Surv.Open一Fide Rep. 87一613,pp146-156.
[9]B F Atwater.  Evidencc for great Holocene earthquakes along the outer coast of Washington state. Science.1987,236,pp942-944.
[10] S R Bartsch-Winkler and H R Schmoll. 1987,Earthquake-caused sedsimentary couplets in the Upper Cook Inlet region,In:T D Hamilton and Geological Survey during 1986. U. S. Geol.Surv. Circular 998, pp92-95.
[11]J Adams.  Paleaseismieity of the Cascadia subduction zone;evidence from Turbidites of the Oregon-Washington margin.Tectonics.1990,pp569-583.
[12]N-A Morner.  Palecselsmieity and Geodynamics in Sweden. Tectonophysics. 1985, 117,pp139-153.
[13]N-A  Morner  et  al.  Neotectonics  and  paleoseismicity  within  the  Stockholm  intracratonal  region  in  Sweden.Tectonophysics. 1989,163,pp289-303.
[14] J Adams.Postglacial faufling in eastern Canada:nature,origin and seismic hazard implications. Tectonophysics. 1989,163,pp323-331.
[15] J Adams. Deformed lake sedimented record prehistoric earthquakes during the deglaciation of  the Canadian shield.EOS.1982,63,pp436.
[16]D Postpischl et al.Paleoseismicity from karst sediments:the "Grotta del Cervo" cave case study (Canadian Italy).Tectonophysics.1991,193,pp141-152.
[17] R S Stein and G C P King. Seismic Potential Revealed by surface folding:1983 Coalinga California:Earthquake,Seience,1984,224,pp869-872.
[18] J D Sims.  Determining earthquake  recurrence  intervals  from deformational  structures in young lacustrine sediments,Tectonophysics.1975,29,pp141-152.
[19]R S Yeats. Coseismic folding.In:Crone A J and Omdahl E M eds.,Directions in paleoseismology,U. S. Geol.Surv.Open-Fide Rep. 1987,87-673,pp163-172.
[20]D P Schwartz and K J Coppersmith.  Fault behavior and characteristic earthquake:examples from the Wasatch and San Andreas fault zones,JGR.1984,89,PP5681-5698.
[21] C H Scholz.  Comments on Models of Earthquake recurrence, In:K. Schwarz and R. H, Sibson eds. proceeding of Conference XLY——Fault Segmentation and Controls of Rupture Initiation and Termination. U. S. Geol. Suev, Open-File Rep.1989,89-315,pp350-360.
[22]K Berryman and S Beanland.  Variation in fault behavriour in different tectonic provinces of New Zealand Journal of Structural Geology,1931,13,pp177-189.