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Crippen, R. E. (1992). Measurement of subresolution terrain displacementsusing SPOT panchromatic imagery. Episodes 15, 56–61.DeMets, C., R. G. Gordon, D. F. Argus, and S. Stein (1994). Effect ofrecent revisions to the geomagnetic reversal time-scale on estimatesof current plate motions. Geophysical Research Letters 21 (20),2,191–2,194.Dorn, C., A. G. Green, R. Jongens, S. Carpentier, A. E. Kaiser, F.Campbell, H. Horstmeyer, J. Campbell, M. Finnemore, andJ. Pettinga (2010). High-resolution seismic images of potentiallyseismogenic structures beneath the northwest CanterburyPlains, New Zealand. Journal of Geophysical Research 115;doi:201010.1029/2010JB007459.Dziewonski, A., T. A. Chou, and J. H. Woodhouse (1981). Determinationof earthquake source parameters from waveform data for studiesof global and regional seismology. Journal of Geophysical Research286, 2,825–2,852.Farr, T., and M. Kobrick (2000). Shuttle Radar Topographic Missionproduces a wealth of data. Eos, Transactions, American GeophysicalUnion 81, 583–585.Fialko, Y., M. Simons, and D. Agnew (2001). The complete (3D) surfacedisplacement field in the epicentral area of the 1999 Mw7.1 Hector Mine Earthquake, California, from space geodeticobservations. Geophysical Research Letters 28 (16), 3,063–3,066;doi:200110.1029/2001GL013174.Fry, B., R. Benites, and A. Kaiser (2011). The character of accelerationsin the M w 6.2 Christchurch earthquake. Seismological ResearchLetters 82, 846–852.Gledhill, K., J. Ristau, M. Reyners, B. Fry, and C. Holden (2011). TheDarfield (Canterbury, New Zealand) Mw 7.1 Earthquake ofSeptember 2010: A Preliminary seismological report. SeismologicalResearch Letters 82 (3), 378–386; doi:10.1785/gssrl.82.6.378.Howard, M., A. Nicol, J. Campbell, and J. R. Pettinga (2005). Holocenepaleoearthquakes on the strike-slip Porters Pass Fault, Canterbury,New Zealand. New Zealand Journal of Geology and Geophysics 48(1), 59–74; doi:10.1080/00288306.2005.9515098.Iizuka, H., Y. Sakai, and K. Koketsu (2011). Strong ground motions anddamage conditions associated with seismic stations in the February2011 Christchurch, New Zealand, earthquake. SeismologicalResearch Letters 82, 875–822.Jackson, J. (1994). Active tectonics of the Aegean region. Annual Reviewof Earth and Planetary Sciences 22 (1), 239–271; doi:10.1146/annurev.ea.22.050194.001323.Kääb, A., and M. Debella-Gilo (2010). Sub-pixel precision image matchingfor measuring surface displacements on mass movements usingnormalized cross-correlation. Remote Sensing of Environment 115(1), 130–142; doi:10.1016/j.rse.2010.08.012.King, G. (2009). Fault interaction, earthquake stress changes, and theevolution of seismicity. In Earthquake Seismology, 225–255, H.Kanamori, ed. Elsevier.Leprince, S., S. Barbot, F. Ayoub, and J.-P. Avouac (2007). Automaticand precise orthorectification, coregistration, and subpixel correlationof satellite images, application to ground deformation measurements.IEEE Transactions on Geoscience and Remote Sensing 45(6), 1,529–1,558; doi:10.1109/TGRS.2006.888937.Lohman, R. B., and W. D. Barnhart (2010). Evaluation of earthquaketriggering during the 2005–2008 earthquake sequenceon Qeshm Island, Iran. Journal of Geophysical Research 115;doi:201010.1029/2010JB007710.Lohman, R. B., and M. Simons (2005). Some thoughts on the use ofInSAR data to constrain models of surface deformation: Noisestructure and data downsampling. Geochemistry GeophysicsGeosystems 6, doi:10.1029/2004GC000841.Mackinnon, T. C. (1983). Origin of the Torlesse terrane and coeval rocks,South Island, New Zealand. Geological Society of America Bulletin94 (8), 967–985; doi:10.1130/0016-7606(1983)942.0.CO;2.Meade, B. J. (2007). Algorithms for the calculation of exact displacements,strains, and stresses for triangular dislocation elements in auniform elastic half space. Computers & Geosciences 33 (8), 1,064–1,075; doi:10.1016/j.cageo.2006.12.003.Melkonian, A. (2011). Measuring glacier velocities and elevation changerates from ASTER data for Juneau icefield, Alaska. Master’s thesis,Cornell University, Ithaca, NY.Michel, R., and J.-P. Avouac (2002). Deformation due to the 17 August 1999Izmit, Turkey, earthquake measured from SPOT images. Journal ofGeophysical Research 107 (B4); doi:10.1029/2000JB000102; http://europa.agu.org/?view=article&uri=/journals/jb/jb0204/2000JB000102/2000JB000102.xml&t=2002. Last accessed June 24, 2011.Norris, R. J., and A. F. Cooper (2001). Late Quaternary slip rates and slippartitioning on the Alpine fault, New Zealand. Journal of StructuralGeology 23 (2–3), 507–520; doi:16/S0191-8141(00)00122-X.Pettinga, J., M. Yetton, R. Van Dissen, and G. Downes (2001).Earthquake source identification and characterization for theCanterbury region, South Island, New Zealand. Bulletin of the NewZealand Society for Earthquake Engineering 34, 282–317.Quigley, M., R. Van Dissen, P. Villamor, N. Litchfield, D. Barrell, K.Furlong et al. (2010). Surface rupture of the Greendale fault duringthe Darfield (Canterbury) earthquake, New Zealand: Initialfindings. Bulletin of the New Zealand Society for EarthquakeEngineering 43 (4), 236–242.Rosen, P. A., S. Hensley, G. Peltzer, and M. Simons (2004). UpdatedRepeat Orbit Interferometry package released. Eos, Transactions,American Geophysical Union 85 (5), 47.Sambridge, M. (1999). Geophysical inversion with a neighbourhoodalgorithm: Searching a parameter space. Geophysical JournalInternational 138 (2), 479–494.Sibson, R., F. Ghisetti, and J. Ristau (2011). Stress control of an evolvingstrike-slip fault system during the 2010–2011 Canterbury, NewZealand, earthquake sequence. Seismological Research Letters 82,824–832.Stirling, M., M. Yetton, J. Pettinga, K. R. Berryman, and G. Downes(1999). Probabilistic Hazard Assessment and Earthquake Scenariosfor the Canterbury Region, and Historic Earthquakes in Christchurch:Stage I (Part B) of Canterbury Regional Council’s Earthquake Hazardand Risk Assessment Study. Canterbury Regional Council ReportNo. U99/18.Sutherland, R., K. Berryman, and R. Norris (2006). Quaternary slip rateand geomorphology of the Alpine fault: Implications for kinematicsand seismic hazard in southwest New Zealand. Geological Societyof America Bulletin 118 (3–4), 464–474; doi:10.1130/B25627.1.Timm, C., K. Hoernle, P. Van Den Bogaard, I. Bindeman, and S. Weaver(2009). Geochemical evolution of intraplate volcanism at BanksPeninsula, New Zealand: Interaction between asthenosphericand lithospheric melts. Journal of Petrology 50 (6), 989–1,023;doi:10.1093/petrology/egp029.Wallace, L. M., J. Beavan, R. McCaffrey, K. Berryman, and P. Denys(2007). Balancing the plate motion budget in the South Island,New Zealand, using GPS, geological and seismological data.Geophysical Journal International 168 (1), 332–352; doi:10.1111/j.1365-246X.2006.03183.x.Wessel, P., and W. H. F. Smith (1998). New, improved version of GenericMapping Tools released. Eos, Transactions, American GeophysicalUnion 79, 579.Department of Earth and Atmospheric SciencesCornell University2120 Snee HallIthaca, New York 14850 U.S.A.wdb47@cornell.edu(W. D. B.)Seismological Research Letters Volume 82, Number 6 November/December 2011 823