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34 results for “fault segmentation”
Supporting Information for "How erosion influence fault segmentation and earthquakes in thrust belts: Low-temperature thermochronology and fluvial shear stress analyses on the southern Longmen Shan, eastern Tibet"
<p>Supporting Information for</p> <p>How erosion influence fault segmentation and earthquakes in thrust belts: Low-temperature thermochronology and fluvial shear stress analyses on the southern Longmen Shan, eastern Tibet</p> <p>Yijia Ye<sup>1</sup>, Xibin Tan<sup>1, </sup>*, Yiduo Liu<sup>2</sup>, Feng Shi<sup>1</sup>, Yuan-Hsi Lee<sup>3</sup>, Michael A. Murphy<sup>2</sup>, Xiwei Xu<sup>4</sup></p> <ol> <li>State Key Laboratory of Earthquake Dynamics, Institute of Geology, China Earthquake Administration, Beijing, 100029, China</li> <li>Department of Earth and Atmospheric Sciences, University of Houston, Houston, TX, 77204-5007, USA</li> <li>Department of Earth and Environmental Sciences, National Chung-Cheng University, Chia-Yi, 62102, Taiwan</li> <li>Institute of Crustal Dynamics, China Earthquake Administration, Beijing, 100085, China</li> </ol> <p><em>* </em>Corresponding author. E-mail address: <a href="mailto:tanxibin@sina.com">tanxibin@sina.com</a></p> <p> </p> <p><strong>Contents of this file </strong></p> <p>Figures S1 and Table S1</p>
Dataset in "Continent-continent Collision between the South and North China Plates Revealed by Seismic Refraction and Reflection at the Southern Segment of the Tanlu Fault Zone""
<p>This dataset contains:</p> <p> Field-data FWI Results<br> Deep Seismic Profiling Result<br> Post-stack Depth Migration<br> Source Signature<br> Misfit Reduction</p> <p>Descriptions:<br> 1. the unit of distance or depth is meter;<br> 2. the unit of time is ms;<br> 3. all the *.dat files are saved as plain text files;<br> 4. all the *.m files are the Matlab scripts for loading and plotting the data.</p>
Late Quaternary slip rate of the Aksay segment and its fast decreasing gradient along the Altyn Tagh fault
<p>Constraining the fault slip rate could reveal the strain accumulation and partitioning pattern. The Aksay segment, the eastern segment of the ATF (Altyn Tagh Fault), as the starting area where the slip rate of ATF decreases, is a strain partitioning zone. The spatial and temporal distribution of fault slip rate along the Aksay segment is of great significance to clarify the role of it in the strain-partitioning of the eastern ATF. We determined the slip rate of four sites along the Aksay segment respectively. The results demonstrated that the slip rate decreased dramatically with an overwhelmingly high slip gradient of ~9.8 mm/yr/100 km within a distance of ~50 km. The slip rate gradient at the Aksay segment is ~4 times of that of the Subei segment to the eastward termination of the ATF. We proposed that the decreased slip rate was absorbed principally by the uplifting of the Danghe Nan Shan. Our results indicated that the slip rate gradient along the ATF was not uniform, and decreased eastward with variable slip rate gradients at different segments, resulting in the uplifting of the mountains oblique with the ATF.</p>
Late Quaternary slip rate of the Aksay segment and its fast decreasing gradient along the Altyn Tagh fault
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The joint inversion results of the receiver functions and apparent S-wave velocities in the central-southern segment of Tanlu fault zone
<p>The folder contains: README, Discontinuities.txt and Velocity_model.</p> <p>README:<br>Description of the data file</p> <p>Discontinuities.txt:<br>This text file contains data related to discontinuities, with the meaning of each column listed in the first row of the file.</p> <p>Velocity_model:<br>This folder contains text files named station names, each representing the inverted velocity model for the corresponding station. The first line of each text file indicates the latitude and longitude of the station. From the second line to the last line, the velocity model is represented as follows: the first column indicates depth, the second column represents Vs (shear wave velocity), the third column indicates the error of Vs, the fourth column represents Vp, and the fifth column indicates the ratio Vp/Vs.</p>
High-resolution lithospheric shear velocity structure of the Suqian segment of the Tanlu fault zone from ambient noise tomography
<p>Our dataset includes S-wave velocity tomography model of of the Suqian segment of the Tanlu fault zone.</p>
Present-day crustal movement and seismic moment balance on major active faults around the easternmost segment of the Kunlun fault, Tibetan Plateau, China
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Spatio-temporal Evolution of Near-field Deformation in Analogue Strike-slip Fault Models with Various Locked Segments Length
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Differential crustal modification mechanism across the central-southern segment of Tanlu fault zone, eastern China
<div> <p>The folder contains: RFs, Discontinuities.txt and Velocity_model.</p> <p>RFs:<br>Receiver function waveforms.</p> <p>Discontinuities.txt:<br>This text file contains data related to discontinuities, with the meaning of each column listed in the first row of the file.</p> <p>Velocity_model:<br>This folder contains text files named station names, each representing the inverted velocity model for the corresponding station. The first line of each text file indicates the latitude and longitude of the station. From the second line to the last line, the velocity model is represented as follows: the first column indicates depth, the second column represents Vs (shear wave velocity), the third column indicates the error of Vs, the fourth column represents Vp, and the fifth column indicates the ratio Vp/Vs.</p> <p> </p> </div>
Teleseismic P-wave data in the Dunhua-Mishan fault (Tanlu northern segment)
<p>Teleseismic P-wave data in the Dunhua-Mishan fault (Tanlu northern segment) </p>
Data of receiver functions in the central and southern segments of the Tanlu fault zone
<p>Data of receiver functions in the central and southern segments of the Tanlu fault zone</p>
Receiver functions of the central and southern segments of the Tanlu fault zone
<p>Data of receiver functions in the central and southern segments of the Tanlu fault zone</p>
Receiver functions of the central and southern segments of the Tanlu fault zone
<p>Data of receiver functions in the central and southern segments of the Tanlu fault zone</p>
Joint Inversion (Receiver function and apparent S-wave velocity) Results of the central-southern segment of Tanlu fault zone
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