[1] Massonnet D, Rossi M, Carmona C, et al. The displacement field of the Landers eartqhuake mapped by radar interferometry[J]. Nature, 1993, 364: 138-142. [2] Goldstein R M, Werner C L. Radar interferogram filtering for geophysical application[J]. Geophysical Research Letters, 1998, 25(21): 4035-4038. [3] Costantini M. A novel phase unwrapping method based on network programming[J]. pdf>. IEEE Transactions on Geoscience and Remote Sensing, 1998, 36(3): 813-821. [4] Rosen P A, Hensley S, Joughin I R, et al. Synthetic aperture radar interferometry[J]. PROCEEDINGS OF THE IEEE, 2000, 88(3): 331-382. [5] Chen C W, Zebker H A. Network approcach to 2D phase unwrapping:intractability and two new algorithms[J]. Journal of the Optical Society of America, 2000, 17(3): 401-414. [6] Chen C W, Zebker H A. Two-dimensional phase unwrapping with use of statistical model for cost functions in nonlinear optimization[J]. J Opt Soc Am, 2001, 18(2): 338-351. [7] Bürgmann R, Rosen P A, Fielding E J. Synthetic Aperture Radar Interferometry to Measure Earth's surface topography and its deformation[J]. Annu Rev Earth Planet, Sci, 2000, 28: 169-209. [8] Hooper A. A multi-temporal InSAR method incorporating both persistent scatterer and small baseline approaches[J]. Geophysical Research Letters, 2008, 35(16), doi: 10.1029/2008gl034654. [9] Hooper A, Segall P, Zebker H. Persistent scatterer interferometric synthetic aperture radar for crustal deformation analysis, with application to Volcán Alcedo, Galápagos[J]. Journal of Geophysical Research, 2007, 112(B7), doi: 10.1029/2006jb004763. [10] Michel R, Jean-PhilippeA vouac. Measuring ground displacements from SAR amplitude images:application to the Landers earthquake[J]. GEOPHYSICAL RESEARCH LETTERS, 1999, 26(7): 875-878. [11] Pathier E, Fielding E J, Wright T J, et al. Displacement field and slip distribution of the 2005 Kashmir earthquake from SAR imagery[J], Geophysical Research Letters, 2006, 33(20), doi:10.1029/2006g1027193. [12] González P J, Fernández J. Error estimation in multitemporal InSAR deformation time series, with application to Lanzarote, Canary Islands[J]. Journal of Geophysical Research, 2011, 116(B10): 561-570. [13] Zebker H A, Rosen P A, Hensley S. Atmospheric effects in interferometric synthetic aperture radar surface deformation and topographic maps[J]. Journal of Geophysical Research, 1997, 102(B4): 7547-7563. [14] Scharroo R, Visser P. Precise orbit determination and gravity field improvement for the ERS statellites[J].pdf>. Journal of Geophysical Research, 1998, 103(C4): 8113-8127. [15] Biggs J, Wright T, Lu Z, et al. Multi-interferogram method for measuring interseismic deformation: Denali Fault, Alaska[J]. Geophysical Journal International, 2007, 170(3): 1165-1179. [16] González P J, Tiampo K F, Camacho A G, et al. Shallow flank deformation at Cumbre Vieja volcano (Canary Islands): Implications on the stability of steep-sided volcano flanks at oceanic islands[J]. Earth and Planetary Science Letters, 2010, 297(3-4): 545-557. [17] Wright T J, Parsons B, England P C, et al. InSAR Observations of low slip rates onthe major faults of Western Tibet[J]. Science, 2004, 305: 236-239. [18] Elliott J R, Biggs J, Parsons B, et al. InSAR slip rate determination on the Altyn Tagh Fault, northern Tibet, in the presence of topographically correlated atmospheric delays[J]. Geophysical Research Letters, 2008, 35(12): 971-989. [19] Cavalié O, Lasserre C, Doin M P, et al. Measurement of interseismic strain across the Haiyuan fault (Gansu, China), by InSAR[J]. Earth and Planetary Science Letters, 2008, 275(3-4): 246-257. [20] Bell M A, Elliott J R, Parsons B E. Interseismic strain accumulation across the Manyi fault (Tibet) prior to the 1997 MW7.6 earthquake[J]. Geophysical Research Letters, 2011, 38(24): 315-331. [21] Wang H, Wright T J, Biggs J. Interseismic slip rate of the northwestern Xianshuihe fault from InSAR data[J]. Geophysical Research Letters, 2009, 36(3), doi:10.1029/2008g1036560. [22] Liu Y, Xu C, Li Z, et al. Interseismic slip rate of the Garze-Yushu fault belt in the Tibetan Plateau from C-band InSAR observations between 2003 and 2010[J]. Advances in Space Research, 2011, 48(12): 2005-2015. [23] Li Z H, Elliott J R, Feng W P, et al. The 2010 MW6.8 Yushu (Qinghai, China) earthquake: Constraints provided by InSAR and body wave seismology[J]. J Geophys Res-Sol Ea, 2011, 116, doi: 10.1029/2011JB008358. [24] Satoshi F, Takuya N, Makoto M, et al. 2.5-D surface deformation of M6.1 earthquake near Mt Iwate detected by SAR interferometry[J]. Geophysical Research Letters, 2000, 27(14): 2049-2052. [25] Tobita M, Nishimura T, Kobayashi T, et al. Estimation of coseismic deformation and a fault model of the 2010 Yushu earthquake using PALSAR interferometry data[J]. Earth and Planetary Science Letters, 2011, 307(3-4), 430-438, doi: 10.1016/j.epsl.2011.05.017. [26] Stramondo S, Kyriakopoulos C, Bignami C, et al. Did the September 2010 (Darfield) earthquake trigger the February 2011 (Christchurch) event?[J]. Science, 2011, 1(98), doi: 10.1038/srep00098. [27] Sigurjon J, Howard Z, Paul S, et al. Fault Slip Distribution of the 1999 MW7.1 Hector Mine, California,Earthquake, Estimated from Satellite Radar and GPS Measurements[J]. Bulletin of the Seismological Society of America, 2002, 92(4): 1377-1389. [28] Ryder I, Parsons B, Wright T J, et al. Post-seismic motion following the 1997 Manyi (Tibet) earthquake: InSAR observations and modelling[J]. Geophysical Journal International, 2007, 169(3): 1009-1027. [29] Wei M, Sandwell D, Smith-Konter B. Optimal combination of InSAR and GPS for measuring interseismic crustal deformation[J]. Advances in Space Research, 2010, 46(2): 236-249, doi: 10.1016/j.asr.2010.03.013.
|