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fault planes) buried in the earth. A tsunami is defined as a series of water waves caused by the displacement of a large volume of a body of water; in the case of this article the body of water being investigated will be a lake rather than an ocean. Also, the focal mechanism plays an important role. Lobes of increased shear stress appear at the fault ends, corresponding to the stress concentrations that tend to extend the fault. The 1.5 m vertical displacement measured by Berberian (1979) provides a constraint for the coseismic slip on the Tabas fold (which is 30% of the total vertical motion), though note that the 1.5 m combines both 35 cm of primary slip, plus cumulative secondary bedding-plane slip. These estimates of fault slip parameters then provide key input into mechanical models of faults and the surrounding crust and upper mantle, estimates of A three-layer elastic-gravitational fault displacement model using dislocation theory has been developed and used to examine the effect of layering of earth elastic moduli on surface and subsurface displacement fields for a vertical strike-slip fault. (1896-1977)International Therefore, it is of value to introduce some terminology with the aim of better describing and distinguishing between such mechanisms. Physics, Astrophysics and AstronomyI have read and accept the Wiley Online Library Terms and Conditions of UseShear concentration in a collision zone: Kinematics of the active Chihshang Fault, Longitudinal Valley, eastern TaiwanActive faulting and earthquake risk: The Chihshang Fault case, TaiwanEffect of baseline corrections on displacements and response spectra for several recordings of the 1999 Chi‐Chi, Taiwan, earthquakeCoseismic and postseismic displacement of the 10 December 2003 (Implications of the rupture process from the displacement distribution of strong motions recorded during the 21 September 1999 Chi‐Chi, Taiwan earthquakeSurface rupture reevaluation of the 1951 earthquake sequence in the central Longitudinal Valley and neotectonic implications (in Chinese with English abstract)Recent faulting in the Longitudinal Valley of eastern TaiwanRelocation of the eastern Taiwan earthquakes and its tectonic implicationsContinuous monitoring of an active fault ina plate‐suture zone: A creepmeter study of the Chihshang active fault, eastern TaiwanActive fault creep variations at Shihshang, Taiwan, revealed by creep meter monitoring, 1998–2001Internal deformation due to shear and tensile faults in a half‐spaceTandem suturing and parting of the Taiwan orogen revealed by its neotectonic elementsGeotectonic evolution of late Cenozoic arc‐continent collision in TaiwanPresent‐day crustal motion along the Longitudinal Valley Fault, eastern TaiwanFault creep on the central segment of the Longitudinal Fault, eastern TaiwanDislocation model for crustal deformation in the Longitudinal Valley area, eastern TaiwanRealization approach of non-linear postseismic deformation model for Taiwan semi-kinematic reference frame, Mixed‐Mode Formation of Amorphous Materials in the Creeping Zone of the Chihshang Fault, Taiwan, and Implications for Deformation Style, New insights into Holocene marine terrace development caused by seismic and aseismic faulting in the Coastal Range, eastern Taiwan, Spatial variation of seismogenic depths of crustal earthquakes in the Taiwan region: Implications for seismic hazard assessment, A mass-wasting dominated Quaternary mountain range, the Coastal Range in eastern Taiwan, Rate‐and‐state friction properties of the Longitudinal Valley Fault from kinematic and dynamic modeling of seismic and aseismic slip, How Well Can We Extract the Permanent Displacement from Low-Cost MEMS Accelerometers?, Long- and short-term triggering and modulation of mud volcano eruptions by earthquakes, Neotectonic characteristics along the eastern flank of the Central Range in the active Taiwan orogen inferred from fluvial channel morphology, Spatiotemporal evolution of seismic and aseismic slip on the Longitudinal Valley Fault, Taiwan, Lithological control on the deformation mechanism and the mode of fault slip on the Longitudinal Valley Fault, Taiwan, A statistical study on ELF‐whistlers/emissions and M ≥ 5.0 earthquakes in Taiwan, Vertical Displacement Rate Field of Taiwan From Geodetic Levelling Data 2000-2008, Seismotectonics of northeastern Taiwan: Kinematics of the transition from waning collision to subduction and postcollisional extension, Monitoring of active tectonic deformations in the Longitudinal Valley (Eastern Taiwan) using Persistent Scatterer InSAR method with ALOS PALSAR data, Postseismic deformation following the 1999 Chi‐Chi earthquake, Taiwan: Implication for lower‐crust rheology, An examination of τc-Pd earthquake early warning method using a strong-motion building array, Tectonic erosion and the removal of forearc lithosphere during arc-continent collision: Evidence from recent earthquake sequences and tomography results in eastern Taiwan, Structure and Holocene evolution of an active creeping thrust fault: The Chihshang fault at Chinyuan (Taiwan), Present‐day kinematics of active mountain building in Taiwan from GPS observations during 1995–2005, Present‐day interseismic surface deformation along the Longitudinal Valley, eastern Taiwan, from a PS‐InSAR analysis of the ERS satellite archives, Residual luminescence in modern debris flow deposits from western Taiwan: A single grain approach, Seismic cycle stress change in western Taiwan over the last 270 years, An automatic scheme for baseline correction of strong-motion records in coseismic deformation determination, Estimation of aseismic crustal-strain using radon precursors of the 2003 M 6.8, 2006 M 6.1, and 2008 M 5.0 earthquakes in eastern Taiwan, Chapter 5 Paleoseismology of Compressional Tectonic Environments, Underground Structural Anomalies and Slow Earthquake Activities Around Seismogenic Megathrust Earthquake Zone as Revealed by Inland Seismic Observations, Complex fault rupture during the 2003 Chengkung, Taiwan earthquake sequence from dense seismic array and GPS observations, Coseismic displacement and tectonic implication of 1951 Longitudinal Valley earthquake sequence, eastern Taiwan, Geomorphology of the southernmost Longitudinal Valley fault: Implications for evolution of the active suture of eastern Taiwan, Seismicity characteristics before the 2003 Chengkung, Taiwan, earthquake, Seismogenic faults along the major suture of the plate boundary deduced by dislocation modeling of coseismic displacements of the 1951 M7.3 Hualien–Taitung earthquake sequence in eastern Taiwan, Approximate recovery of coseismic deformation from Taiwan strong-motion records, Seismic tomography of Taiwan: Improved constraints from a dense network of strong motion stations, Coseismic source model of the 2003 M 6.8 Chengkung earthquake, Taiwan, determined from GPS measurements, Seismogenic structure in a tectonic suture zone: With new constraints from 2006 Mw6.1 Taitung earthquake, Very low frequency earthquakes within accretionary prisms are very low stress‐drop earthquakes,

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