Geodetic Constraints of the 2017 Mw7.3 Sarpol Zahab, Iran Earthquake, and Its Implications on the Structure and Mechanics of the Northwest Zagros Thrust‐Fold Belt

[1]  M. Tatar,et al.  The 2013 Mw 6.2 Khaki‐Shonbe (Iran) Earthquake: Insights into seismic and aseismic shortening of the Zagros sedimentary cover , 2015 .

[2]  Sergey V. Samsonov,et al.  A Slip Gap of the 2016 Mw 6.6 Muji, Xinjiang, China, Earthquake Inferred from Sentinel‐1 TOPS Interferometry , 2017 .

[3]  Y. Fialko.  Probing the mechanical properties of seismically active crust with space geodesy: Study of the coseismic deformation due to the 1992 Mw7.3 Landers (southern California) earthquake , 2004 .

[4]  Shahriar Sadeghi,et al.  Spatial evolution of Zagros collision zone in Kurdistan, NW Iran: constraints on Arabia–Eurasia oblique convergence , 2015 .

[5]  Stephen B. DeLong,et al.  Afterslip Behavior following the 2014 M 6.0 South Napa Earthquake with Implications for Afterslip Forecasting on Other Seismogenic Faults , 2016 .

[6]  James Jackson,et al.  The accommodation of Arabia‐Eurasia Plate convergence in Iran , 1995 .

[7]  Thrust Systems.  THRUST SYSTEMS , 2017 .

[8]  Paul Tapponnier,et al.  Structural segmentation controlled the 2015 Mw 7.8 Gorkha earthquake rupture in Nepal , 2016 .

[9]  A. Copley.  Postseismic afterslip 30 years after the 1978 Tabas-e-Golshan (Iran) earthquake: observations and implications for the geological evolution of thrust belts , 2014 .

[10]  Frederic Masson,et al.  Seismic versus aseismic deformation in Iran inferred from earthquakes and geodetic data , 2004 .

[11]  Yehuda Bock,et al.  Localized and distributed creep along the southern San Andreas Fault , 2014 .

[12]  C. Werner,et al.  Sentinel-1 support in the GAMMA Software , 2015 .

[13]  Abbas Bahroudi,et al.  The 18 August 2014 Mw 6.2 Mormori, Iran, Earthquake: A Thin‐Skinned Faulting in the Zagros Mountain Inferred from InSAR Measurements , 2015 .

[14]  Walter H. F. Smith,et al.  New, improved version of generic mapping tools released , 1998 .

[15]  Sergey V. Samsonov,et al.  Seismogenic faulting of the sedimentary sequence and laterally variable material properties in the Zagros Mountains (Iran) revealed by the August 2014 Murmuri (E. Dehloran) earthquake sequence , 2015 .

[16]  T. Farr,et al.  Shuttle radar topography mission produces a wealth of data , 2000 .

[17]  O. Lacombe,et al.  Building the Zagros collisional orogen: Timing, strain distribution and the dynamics of Arabia/Eurasia plate convergence , 2012 .

[18]  Yehuda Bock,et al.  Parkfield earthquake: Stress-driven creep on a fault with spatially variable rate-and-state friction parameters , 2009 .

[19]  Rowena B. Lohman,et al.  Some thoughts on the use of InSAR data to constrain models of surface deformation: Noise structure and data downsampling , 2005 .

[20]  B. E. Shaw,et al.  Afterslip and aftershocks in the rate‐and‐state friction law , 2007, physics/0703249.

[21]  Ian Parsons,et al.  Surface deformation due to shear and tensile faults in a half-space , 1986 .

[22]  F. Wan,et al.  Fault parameters of the October 2008 Damxung Mw6.3 earthquake from InSAR inversion and its tectonic implication , 2010 .

[23]  Emma M. Hill,et al.  The mechanism of partial rupture of a locked megathrust: The role of fault morphology , 2016 .

[24]  Remko Scharroo,et al.  Generic Mapping Tools: Improved Version Released , 2013 .

[25]  Sergey V. Samsonov,et al.  Multidimensional time‐series analysis of ground deformation from multiple InSAR data sets applied to Virunga Volcanic Province , 2012 .

[26]  Frederic Masson,et al.  Present‐day crustal deformation and plate kinematics in the Middle East constrained by GPS measurements in Iran and northern Oman , 2004 .

[27]  P. Bird.  An updated digital model of plate boundaries , 2003 .

[28]  M. Berberian.  Master “blind” thrust faults hidden under the Zagros folds: active basement tectonics and surface morphotectonics , 1995 .

[29]  Marion Y. Thomas,et al.  Time-dependent postseismic slip following the 1978 M w 7.3 Tabas-e-Golshan, Iran earthquake revealed by over 20 years of ESA InSAR observations , 2018 .

[30]  James J. Lienkaemper,et al.  Long‐Term Afterslip of the 2004 M 6.0 Parkfield, California, Earthquake—Implications for Forecasting Amount and Duration of Afterslip on Other Major Creeping Faults , 2017 .

[31]  J. Dieterich.  Earthquake nucleation on faults with rate-and state-dependent strength , 1992 .

[32]  M. Tatar,et al.  New views on earthquake faulting in the Zagros fold-and-thrust belt of Iran , 2011 .

[33]  Kristine M. Larson,et al.  Frictional Properties on the San Andreas Fault near Parkfield, California, Inferred from Models of Afterslip following the 2004 Earthquake , 2006 .