Interseismic Kinematics Along the Tuolaishan-Lenglongling Fault Determined by Sentinel-1 Insar Observations

[1]  G. Feng,et al.  Coseismic Kinematics of the 2023 Kahramanmaras, Turkey Earthquake Sequence From InSAR and Optical Data , 2023, Geophysical Research Letters.

[2]  Peizhen Zhang,et al.  Along-strike variation in fault structural maturity and seismic moment deficits on the Yushu-Ganzi-Xianshuihe fault system revealed by strain accumulation and regional seismicity , 2022, Earth and Planetary Science Letters.

[3]  Teng Wang,et al.  Strain Partitioning on the Western Haiyuan Fault System Revealed by the Adjacent 2016 Mw5.9 and 2022 Mw6.7 Menyuan Earthquakes , 2022, Geophysical Research Letters.

[4]  Qiang Li,et al.  Coseismic Rupture Model and Tectonic Implications of the January 7 2022, Menyuan Mw 6.6 Earthquake Constraints from InSAR Observations and Field Investigation , 2022, Remote. Sens..

[5]  Peizhen Zhang,et al.  Kinematics of the ∼1000 km Haiyuan fault system in northeastern Tibet from high-resolution Sentinel-1 InSAR velocities: Fault architecture, slip rates, and partitioning , 2022, Earth and Planetary Science Letters.

[6]  Jihong Liu,et al.  Three-Dimensional Surface Displacements of the 8 January 2022 Mw6.7 Menyuan Earthquake, China from Sentinel-1 and ALOS-2 SAR Observations , 2022, Remote. Sens..

[7]  T. Wright,et al.  Large‐Scale Interseismic Strain Mapping of the NE Tibetan Plateau From Sentinel‐1 Interferometry , 2022, Journal of Geophysical Research: Solid Earth.

[8]  Jihong Liu,et al.  Surface Displacement and Source Model Separation of the Two Strongest Earthquakes During the 2019 Ridgecrest Sequence: Insights From InSAR, GPS, and Optical Data , 2022, Journal of Geophysical Research: Solid Earth.

[9]  Dun Wang,et al.  Rapid report of the 8 January 2022 Ms 6.9 Menyuan earthquake, Qinghai, China , 2022, Earthquake Research Advances.

[10]  R. Bürgmann,et al.  Large‐Scale Crustal Deformation, Slip‐Rate Variation, and Strain Distribution Along the Kunlun Fault (Tibet) From Sentinel‐1 InSAR Observations (2015–2020) , 2022, Journal of Geophysical Research: Solid Earth.

[11]  Jihong Liu,et al.  Coseismic and Early Postseismic Slip Models of the 2021 Mw 7.4 Maduo Earthquake (Western China) Estimated by Space‐Based Geodetic Data , 2021, Geophysical Research Letters.

[12]  Yunmeng Cao,et al.  Interseismic Deformation From Sentinel‐1 Burst‐Overlap Interferometry: Application to the Southern Dead Sea Fault , 2021, Geophysical Research Letters.

[13]  J. Nocquet,et al.  Geodetic Observations of Shallow Creep on the Laohushan‐Haiyuan Fault, Northeastern Tibet , 2021, Journal of Geophysical Research: Solid Earth.

[14]  Qin Zhang,et al.  Sentinel-1 InSAR observations of co- and post-seismic deformation mechanisms of the 2016 Mw 5.9 Menyuan Earthquake, Northwestern China , 2021 .

[15]  G. Feng,et al.  Pre- and post-failure spatial-temporal deformation pattern of the Baige landslide retrieved from multiple radar and optical satellite images , 2020 .

[16]  Zhujun Han,et al.  A New Tectonic Model for the 1927 M8.0 Gulang Earthquake on the NE Tibetan Plateau , 2020, Tectonics.

[17]  Yingfeng Zhang,et al.  The 2016 Mw 5.9 Menyuan Earthquake in the Qilian Orogen, China: A Potentially Delayed Depth-Segmented Rupture Following from the 1986 Mw 6.0 Menyuan Earthquake , 2020 .

[18]  Zheng‐Kang Shen,et al.  Present‐Day Crustal Deformation of Continental China Derived From GPS and Its Tectonic Implications , 2020, Journal of Geophysical Research: Solid Earth.

[19]  Zhi‐wei Li,et al.  Source parameters and slip distribution of the 2018 M 7.5 Palu, Indonesia earthquake estimated from space-based geodesy , 2019 .

[20]  Xiaoli Ding,et al.  Complete Three‐Dimensional Coseismic Deformation Field of the 2016 Central Tottori Earthquake by Integrating Left‐ and Right‐Looking InSAR Observations With the Improved SM‐VCE Method , 2019, Journal of Geophysical Research: Solid Earth.

[21]  D. Sandwell,et al.  Slow Slip Event On the Southern San Andreas Fault Triggered by the 2017 Mw8.2 Chiapas (Mexico) Earthquake , 2019, Journal of Geophysical Research: Solid Earth.

[22]  Yu Jiang,et al.  A Fine Velocity and Strain Rate Field of Present-Day Crustal Motion of the Northeastern Tibetan Plateau Inverted Jointly by InSAR and GPS , 2019, Remote. Sens..

[23]  Yingfeng Zhang,et al.  Source parameters of the 2016 Menyuan earthquake in the northeastern Tibetan Plateau determined from regional seismic waveforms and InSAR measurements , 2018, Journal of Asian Earth Sciences.

[24]  Chisheng Wang,et al.  Elastic block and strain modeling of GPS data around the Haiyuan-Liupanshan fault, northeastern Tibetan Plateau , 2017 .

[25]  Yidong Lou,et al.  Crustal Deformation in the India‐Eurasia Collision Zone From 25 Years of GPS Measurements , 2017 .

[26]  Zhujun Han,et al.  Slip rate and recurrence intervals of the east Lenglongling fault constrained by morphotectonics: Tectonic implications for the northeastern Tibetan Plateau , 2017 .

[27]  W. Feng,et al.  Activity of the Lenglongling fault system and seismotectonics of the 2016 MS6.4 Menyuan earthquake , 2017, Science China Earth Sciences.

[28]  Yongsheng Li,et al.  Space Geodetic Observations and Modeling of 2016 Mw 5.9 Menyuan Earthquake: Implications on Seismogenic Tectonic Motion , 2016, Remote. Sens..

[29]  W. Gan,et al.  Deformation of the Haiyuan-Liupanshan fault zone inferred from the denser GPS observations , 2015 .

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

[31]  Marie-Pierre Doin,et al.  Spatio-temporal evolution of aseismic slip along the Haiyuan fault, China: Implications for fault frictional properties , 2013 .

[32]  Marie-Pierre Doin,et al.  Shallow creep on the Haiyuan Fault (Gansu, China) revealed by SAR Interferometry , 2012 .

[33]  Peizhen Zhang,et al.  Transformation of displacement between strike-slip and crustal shortening in the northern margin of the Tibetan Plateau: Evidence from decadal GPS measurements and late Quaternary slip rates on faults , 2011 .

[34]  Henriette Sudhaus,et al.  Source model for the 1997 Zirkuh earthquake (MW = 7.2) in Iran derived from JERS and ERS InSAR observations , 2011 .

[35]  Marie-Pierre Doin,et al.  Measurement of interseismic strain across the Haiyuan fault (Gansu, China), by InSAR , 2008 .

[36]  Peizhen Zhang,et al.  Present‐day crustal motion within the Tibetan Plateau inferred from GPS measurements , 2007 .

[37]  Yuri Fialko,et al.  Structure and mechanical properties of faults in the North Anatolian Fault system from InSAR observations of coseismic deformation due to the 1999 Izmit (Turkey) earthquake , 2007 .

[38]  David A. Seal,et al.  The Shuttle Radar Topography Mission , 2007 .

[39]  M. Caffee,et al.  Fast late Pleistocene slip rate on the Leng Long Ling segment of the Haiyuan fault, Qinghai, China , 2002 .

[40]  L. B. Freund,et al.  A two-dimensional analysis of surface deformation due to dip-slip faulting , 1976 .

[41]  J. C. Savage,et al.  Geodetic determination of relative plate motion in central California , 1973 .

[42]  H. Wanga,et al.  Sentinel-1 observations of the 2016 Menyuan earthquake : A buried reverse event linked to the left-lateral Haiyuan fault , 2017 .

[43]  L. Hao,et al.  Determination of the Slip Rate of the Lenglongling Fault in the Middle and Eastern Segments of the Qilian Mountain Active Fault Zone , 2010 .

[44]  C. Werner,et al.  GAMMA SAR AND INTERFEROMETRIC PROCESSING SOFTWARE , 2000 .

[45]  H. Wen RESEARCH ON SLIP RATES OF THE LENGLONGLING ACTIVE FAULT ZONE , 2000 .