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11 results for “post-seismic”

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zenodo44/100

VEL-Ar trajectory prediction model linear, co-seismic, and post-seismic grids for interpolation

<p>VEL-Ar trajectory prediction model linear, co-seismic, and post-seismic interpolation grids in ASCII format. The generation of these grids is described in http://doi.org/10.1007/s00190-015-0871-8</p>

opencc-by-4.0Dec 2015View details →
zenodo40/100

Earthquake Catalogue for: Illuminating the pre-, co-, and post-seismic phases of the 2016 M7.8 Kaikoura earthquake with 10 years of seismicity

<p><strong>0.2: Correction</strong></p> <p>This version corrects the original dataset which had some incorrect focal mechanisms. These mechanisms had incorrect rakes as a result of an error in the uncertainty calculation algorithm. The remainder of the catalogue is unchanged.</p> <p><strong>Code:</strong></p> <p>If you are looking for the code used for this project this is here: <a href="https://zenodo.org/record/5047794#.Y22Mvn5By-Y">https://zenodo.org/record/5047794#.Y22Mvn5By-Y</a> - the link in the paper appears to be wrong as of 11/11/2022.</p> <p><strong>Description</strong></p> <p>Earthquake catalogue generated around the rupture area of the 2016 M7.8 Kaikoura earthquake. For a full description see the associated paper submitted to JGR 2021.</p> <p>The catalogue is here in two forms:</p> <ol> <li>A QuakeML file with all picks, magnitudes, and locations included. This is quite a large file. When reading using ObsPy this will take a long time to read (&gt;10 minutes), and expand in memory to &gt; 8GB.</li> <li>A CSV file with the preferred origin and magnitude information for all events. Relocated events can be identified because they have a station count of 0: GrowClust does not return the number of stations used, whereas NonLinLoc (used for absolute locations) does.</li> </ol>

opencc-by-4.0Apr 2021View details →
zenodo40/100

Controls on post-seismic landslide behaviour in brittle rocks - Datasets

<p>Datasets summarising:</p> <p>1. DynBPS direct shear data;</p> <p>2. physical properties of the Tubul Sandstone analysed; and</p> <p>3.&nbsp;&nbsp;post-shear height profiles along samples, derived from Structure-from-Motion photogrammetry.</p>

opencc-by-4.0Jul 2021View details →
zenodo36/100

Co- and Post-seismic Crustal Deformation Associated with the 2016 Kumamoto Earthquake Sequence Revealed by PALSAR-2 Pixel Tracking and InSAR

<p>This archive includes the dataset for the co- and post-seismic displacements associated with the 2016 Kumamoto earthquake in Japan detected by ALOS-2/PALSAR-2 data. All files are formatted as the MATLAB format. ALOS-2/PALSAR-2 level 1.1 data in this study were provided from the PIXEL (PALSAR Interferometry Consortium to Study our Evolving Land Surface) under a cooperative research contract with the Earthquake Research Institute, University of Tokyo. The ownership of ALOS-2/PALSAR-2 level 1.1 data belongs to JAXA.</p> <p>&nbsp;</p> <p>coseismic_datav1.mat contains the original PALSAR-2 pixel tracking data and 3D displacement components. You can display 3D displacement field using &quot;display_3Ddisp.m&quot;.</p> <p>coseismc_flocv1.mat contains the isolated displacement discontinuities in the observation data.</p> <p>postseismic_asc_v1.mat contains the PALSAR-2 original InSAR data in the ascending orbit.</p> <p>postseismic_dsc_v1.mat contains the PALSAT-2 original InSAR data in the descending orbit.</p> <p>script_acrossp_p.m generates the profiles of post-seismic displacement profile across the profile.</p> <p>script_alongp_c.m generates the profiles of co-seismic displacement along the fault.</p> <p>script_alongp_p.m generates the profiles of post-seismic displacement along the fault.</p> <p>script_quasi_def.m generates the quasi-eastwest and the quasi-vertical displacement fields.</p> <p>script_ts.m generates the time-series of line-of-sight change using the sequence of InSAR data.</p> <p>-</p> <p>display_3Ddisp.m displays 3D displacement fields using &quot;coseismic_datav1.m&quot;.</p> <p>coseis_Fdisp.mat contains data for along-fault displacement. (Lon, Lat, vertical, stv_vertical, horizontal_alongfault, stv_horizontal_alongfault, and topography)</p> <p>display_coseis_alongdisp.m generates figures for the along-fault displacement distribution using &quot;coseis_Fdisp.mat&quot;.</p>

opencc-by-4.0Apr 2020View details →
zenodo36/100

Co-seismic and post-seismic differential Interferograms and displacement maps for the 2020 M6.5 Monte Cristo Range, Nevada earthquake

<p>Differential interferograms for the Mw 6.5 Monte Cristo, Nevada earthquake, processed with SNAP and CNR-IREA P-SBAS in the <a href="https://geohazards-tep.eu">Geohazards Exploitation Platform</a>.</p> <p>USGS event page for the Monte Cristo earthquake:</p> <p><a href="https://earthquake.usgs.gov/earthquakes/eventpage/nn00725272/">https://earthquake.usgs.gov/earthquakes/eventpage/nn00725272/</a></p> <p>Co-seismic and post-seismic (May 16 - May 23) interferograms are included. For each interferometric pair, three products are included: coherence, phase interferogram and unwrapped interferogram (LOS displacement). Decomposition.zip files includes the processed East-West and Vertical deformation maps from combining ascending and descending interferograms.</p> <p>&nbsp;</p>

opencc-by-4.0Nov 2020View details →
zenodo36/100

InSAR time-series and FEM Model of the Post-seismic Surface Deformation following the 2013 Baluchistan Earthquake

<p>Subduction zone accretionary prisms are commonly modeled as elastic structures where permanent deformation is accommodated by faulting and folding of otherwise elastic materials, yet accretionary prisms may exhibit other deformation styles over relatively short time scales. In this study, we use 6.5-year (2014-2021) Sentinel-1 InSAR time-series of post-seismic deformation in the Makran accretionary prism of southeast Pakistan to characterize non-linear viscoelastic deformation within an active accretionary prism on short timescales (months to years). We constructed a series of 3-D finite-element models of the Makran subduction zone, including an accretionary prism, and constrained the elastic thickness of the upper wedge and the flow-law parameters (power-law exponent, activation enthalpy, and pre-exponential constant) of the lower wedge through forward model fits to the InSAR time-series. Our results show that the prism is elastically thin (8-12 km) and the non-linear viscoelastic relaxation of the deep portions of the prism alone can sufficiently explain the post-seismic surface deformation. Our best fitting flow-law parameters (<em>n</em> = 3.76&plusmn;0.39, <em>Q</em> = 82.2&plusmn;37.73 kJ mol<sup>-1</sup>, and <em>A</em> = 10<sup>-3.36&plusmn;4.69</sup>) are consistent with triggering of low temperature dislocation creep within fluid-saturated siliciclastic rocks. We believe that the fluids necessary for this weakening originate from sedimentary underplating and/or the presence the hydrocarbons. The presence of power-law rheology within the lower wedge impacts the estimated plate coupling and the stress state in the subduction system, with respect to the conventional elastic wedge model, and hence need to be considered in future earthquake cycle models.</p>

opencc-by-4.0Oct 2022View details →
zenodo32/100

Evolution of coseismic and post-seismic landsliding after the 2015 Mw 7.8 Gorkha earthquake, Nepal

<p>Landslide area density grid used in the analysis of the spatial evolution of landsliding following the 2015 Mw 7.8 Gorkha earthquake in Nepal. The data include 11 epochs of landslide area density, including bi-annual assessments between 2014 and 2018 (pre- and post-monsoon), and an additional coseismic assessment from 2015.&nbsp;</p> <p>This&nbsp;research has been supported by the UKRI-DFID SHEAR program (201844-112).&nbsp;</p>

opencc-by-4.0Nov 2020View details →
zenodo32/100

Supplementary materials for an AI-based method for estiamting the potential runout distance of post-seismic debris flows

<p>We included several figures and tables in this file to support the study on runout distance estimation using a AI-based method, mainly focusing on the precipitation downscaling, calibration, assessment, and rainfall threshold calculation. Additionally, the prediction results of all the debris flow catchments were included in a table when intraday rainfall ranges from 40 to 100 mm.</p>

opencc-by-4.0Jul 2024View details →
zenodo32/100

Figures for "New method for computing post-seismic deformations in a realistic gravitational viscoelastic Earth model"

<p>Here are all the figures used in the paper &quot;New method for computing post-seismic deformations in a realistic gravitational viscoelastic Earth model&quot;.&nbsp;</p>

opencc-by-4.0Jan 2019View details →
zenodo32/100

All figures for "Application of a new method to simulate post-seismic deformations in a realistic Earth model"

<p>It is a zip file for the figures used in paper&nbsp;&quot;Application of a new method to simulate &nbsp;post-seismic deformations in a realistic Earth model&quot;.</p>

opencc-by-4.0Oct 2019View details →
zenodo28/100

The coseismic and post-seismic deformation of 2020 Nima earthquake obatined by InSAR

<p>The two zip files contain the co-seismic deformation and accumulated post-seismic deformation (line of sight ) of ascending and descending orbits of the 2020 Nima earthquake observed by Sentinel-1. The units of co-seismic and post-seismic deformation are meter and millimeter respectively. The positive value is motions to the satellite, and the negative value is motins away from the satellite.</p> <p>If you have any questions about this data, please contact me via <a href="mailto:gaohuastudent@163.com">gaohuastudent@163.com</a>.</p>

opencc-by-4.0May 2021View details →

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