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488 results for “Rupture”

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zenodo36/100

Fault zone material files for dynamic rupture modeling of the 2019 Ridgecrest earthquakes

<p>This repository contains the material files used to add a low-velocity fault zone to a dynamic rupture model of the 2019 Ridgecrest sequence (Taufiqurrahman et al., 2023, Nature).</p>

opencc-by-4.0Nov 2024View details →
zenodo36/100

Relationship between rupture length and magnitude of oceanic transform fault earthquakes

<p>We provide here the supplementary material to&nbsp;<em><strong>Relationship between rupture lengths and magnitudes of oceanic transform fault earthquakes,</strong>&nbsp;</em>by&nbsp;Guilherme de Melo, Ingo Grevemeyer, Dietrich Lange, Dirk Metz, and Heidrun Kopp.</p> <p>&nbsp;</p>

opencc-by-4.0Dec 2024View details →
zenodo36/100

Data Set of Publication - Outcome of Scleral Rupture Primary Management Without Vitrectomy Jakarta Eye Trauma Study

<p>This dataset was collected for research purposes. The dataset was about the scleral rupture we found in our teritories</p>

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

SeisSol input files for the dynamic rupture scenarios based on the 2004 Sumatra-Andaman earthquake published in Madden et al. (2022) "The state of pore fluid pressure and 3D megathrust earthquake dynamics" JGR-Solid Earth

<p>This dataset contains the input files of the dynamic&nbsp;rupture scenarios from&nbsp;Madden, E. H., T. Ulrich and A.-A. Gabriel&nbsp;(2022), The State of Pore Fluid Pressure and 3-D Megathrust Earthquake Dynamics, Journal of Geophysical Research-Solid Earth,&nbsp;<a href="https://doi.org/10.1029/2021JB023382">https://doi.org/10.1029/2021JB023382</a>.&nbsp;(Earlier preprint available at: <a href="https://doi.org/10.1002/essoar.10508297.1">https://doi.org/10.1002/essoar.10508297.2</a>)</p> <p><strong>easi/yaml parameter files for the 6 scenarios studied:&nbsp;</strong><br> PAR_Sumatra_scen1new_gen.par,&nbsp;PAR_Sumatra_scen2new_gen.par,&nbsp;PAR_Sumatra_scen3new_gen.par,&nbsp;PAR_Sumatra_scen4new_gen.par,&nbsp;PAR_Sumatra_scen5new_gen.par,&nbsp;PAR_Sumatra_scen6new_gen.par</p> <p><strong>easi/yaml files setting initial on-fault friction, stress and pore fluid pressure conditions for the 6 scenarios studied:&nbsp;</strong>iniStress_Sumatra_scen1new.yaml,&nbsp;iniStress_Sumatra_scen2new.yaml,&nbsp;iniStress_Sumatra_scen3new.yaml,&nbsp;iniStress_Sumatra_scen4new.yaml,&nbsp;iniStress_Sumatra_scen5new.yaml,&nbsp;iniStress_Sumatra_scen6new.yaml<br> <br> <strong>easi/yaml file&nbsp;describing the rock elastic properties in all 6 scenarios:</strong>&nbsp;<br> matprops_Sumatra_2019_LVZ.yaml<br> <br> <strong>mesh file:</strong>&nbsp;<br> topo4_splays_fix9-14.1e6-28m.dtc1-v2-suma</p> <p>&nbsp;</p>

opencc-by-4.0Jan 2022View details →
zenodo36/100

Line-Source Model based Rapid Inversion for Deriving Large Earthquake Rupture Characteristics using High-rate GNSS Observations

<p>The high-rate GNSS data and GNSS-derived velocity waveforms of six&nbsp;large earthquakes (the 2016 Mw 6.6 Norcia earthquake, the 2010 Mw 7.2 EI Mayor-Cucapah earthquake, the 2016 Mw 7.8 Kaikoura earthquake, the 2019 Mw 7.1 Ridgecrest earthquake, the 2014 Mw 8.2 Iquique earthquake, and the 2015 Mw 8.3 Illapel earthquake) are&nbsp;included in this&nbsp;repository.</p>

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

Map and offsets of the Ar-Hötöl surface rupture along the Khovd fault (Mongolian Altay)

<p><strong>Detailed map of the surface ruptures and affected geomorphological markers for the Ar-Khutul section of the Khovd Fault in the Mongolian Altay. Observations are based on a multi-scale approach combining a range of airborne and terrestrial imaging and topographic techniques: Sentinel-2, Pleiades, TanDEM-X, UAV, and terrestrial laser scanning. This dataset is composed of a detailed map of tectonic scarps with a distribution of offset values below 10 m.</strong></p>

opencc-by-4.0Feb 2022View details →
zenodo36/100

On the scale dependence in the dynamics of frictional rupture: constant fracture energy versus size-dependent breakdown work

<pre>Potential energy stored during the inter-seismic period by tectonic loading around faults is released during earthquakes as radiated energy, frictional dissipation and fracture energy. The latter is of first importance since it is expected to control the nucleation, the propagation and the arrest of the seismic rupture. On one side, the seismological fracture energy estimated for natural earthquakes (commonly called breakdown work) ranges between 1 $\mathrm{J/m^2}$ and tens of $ \mathrm{MJ/m^2} $ for the largest events, and shows a clear slip dependence. On the other side, recent experimental studies highlighted that, concerning rupture experiments, fracture energy is a material property (energy required to break the fault interface) independently of the size of the event, i.e. of the seismic slip. </pre> <pre>To reconcile these contradictory observations and definitions, we performed stick-slip experiments, as analog for earthquakes, in a bi-axial shear configuration. We estimated fracture energy through both Linear Elastic Fracture Mechanics (LEFM) and a Cohesive Zone Model (CZM) and through the integration of the near-fault stress-slip evolution. We show that, at the scale of our experiments, fault weakening is divided into a near-tip weakening, corresponding to an energy of few $ \mathrm{J/m^2} $, consistent with the one estimated through LEFM and CZM, and a long-tailed weakening corresponding to a larger energy not localized at the rupture tip, increasing with slip.</pre> <pre>Through numerical simulations, we demonstrate that only near-tip weakening controls the rupture initiation and that long-tailed weakening can enhance slip during rupture propagation and allow the rupture to overcome stress heterogeneity along the fault. We conclude that the origin of the seismological estimates of breakdown work could be related to the energy dissipated in the long-tailed weakening rather than to the one dissipated near the tip.</pre>

opencc-by-4.0Feb 2022View details →
zenodo36/100

Dataset for manuscript Precursor-free eruption triggered by edifice rupture at Nyiragongo volcano

<p>This archive file contains datafiles used in &quot;Precursor-free eruption triggered by edifice rupture at Nyiragongo volcano&quot; manuscript.&nbsp;</p> <p>i.e. : Ash Index, Lava flow shp, fractures shp, eruptive fissure shp, GNSS, InSAR, Seismic catalog, SO2 measurmement and Dike Modeling inputs and results.</p>

opencc-by-4.0May 2022View details →
zenodo36/100

Fault strength and rupture process controlled by fault surface topography

<p>Experimental source data for the study &quot;Fault strength and rupture process controlled by fault surface topography&quot;</p>

opencc-by-4.0Sep 2022View details →
zenodo36/100

Supplementary dataset for " Kinematic rupture modeling of broadband ground motion from the 2022 MS6.9 Menyuan earthquake"

<p>This is the data used in&nbsp;&quot; Kinematic rupture modeling of broadband ground motion from the 2022 MS6.9 Menyuan earthquake&quot;. The paper is currently under review.</p>

opencc-by-4.0Oct 2022View details →
zenodo36/100

Earthquake Cycle Deformation Associated with the 2021 Mw 7.4 Maduo (Eastern Tibet) Earthquake: An Intrablock Rupture Event on a Slow-Slipping Fault from Sentinel-1 InSAR and Teleseismic Data

<p>Coseismic slip models of the 2021&nbsp;Mw 7.4 Maduo (eastern Tibet) earthquake derived from Sentinel-1 InSAR and teleseismic data.</p> <p>Interseismic eastward and vertical velocity and maximum shear strain rate fields.</p> <p>Citations:</p> <p>Fang, J., Ou, Q., Wright, T. J., Okuwaki,&nbsp;R., Amey, R. M. J., Craig, T. J., et al.&nbsp;(2022). Earthquake cycle deformation&nbsp;associated with the 2021 M<span>W </span>7.4 Maduo&nbsp;(eastern Tibet) earthquake: An intrablock&nbsp;rupture event on a slow-slipping fault&nbsp;from Sentinel-1 InSAR and teleseismic&nbsp;data. Journal of Geophysical Research:&nbsp;Solid Earth, 127, e2022JB024268. <span>https://</span>doi.org/10.1029/2022JB024268</p> <p>Fang, J., Ou, Q., Wright, T. J., Okuwaki,&nbsp;R., Amey, R. M. J., Craig, T. J., et al.&nbsp;(2022). Earthquake cycle deformation&nbsp;associated with the 2021 M<span>W </span>7.4 Maduo (eastern Tibet) earthquake: An intrablock rupture event on a slow-slipping fault from Sentinel-1 InSAR and teleseismic data [Data set]. Zenodo.&nbsp;https://doi.org/10.5281/zenodo.7215161<span>.</span></p>

opencc-by-4.0Oct 2022View details →
zenodo36/100

numerical data to accompany "Strong asymmetry in near-fault ground velocity during an oblique strike-slip earthquake revealed by waveform particle motions and dynamic rupture simulations"

<p>This is the numerical data to accompany the paper "Strong asymmetry in near-fault ground velocity during an oblique strike-slip earthquake revealed by waveform particle motions and dynamic rupture simulations". Please refer to the README.txt file for information about the individual datasets and archive files.&nbsp;</p>

opencc-by-4.0Dec 2023View details →
zenodo36/100

Data for "effects of fault contact heterogeneity on laboratory earthquake initiation and dynamic rupture"

<p>The second column in the files named by "Time_and_dLP", "Time_and_Mu0", "Time_and_Sigma0", and "Time_and_Tau0" indicate the along-fault loading point displacement (dLP), macroscopic friction coefficient (Mu0), macroscopic normal stress (Sigma0), and macroscopic shear stress (Tau0), respectively, measured in the loading apparatus. The first column in these files are time.</p> <p>Local fault displacement data are named by the form of, for example, "Event101_FaultDisplacement_L1(x=270mm)", which means that the fault displacement measured by Sensor L1 located at x=270 mm during stick-slip Event 101. Their corresponding time is save in the file named by "Event101_FaultDisplacement_Time".</p> <p>Local shear stress data are named by the form of, for example, "Event101_ShearStress_S1(x=-323.95mm)", which means that the shear stress measured by Sensor S1 located at x=-323.95 mm during stick-slip Event 101. Their corresponding time is save in the file named by "Event101_ShearStress_Time".</p>

opencc-by-4.0Jun 2024View details →
zenodo36/100

Thrust-dominated unilateral rupture of a blind listric fault associated with the 2024 Hualien earthquake

<p>Slip model and the interferometric synthetic aperture radar (InSAR) of the 2024 Hualian Mw 7.4 earthquake.</p>

opencc-by-4.0Jul 2024View details →
zenodo36/100

Electronic Supplement to Structural configuration of the Otates fault (southern Basin-and-Range Province) and its rupture in the 3 May 1887 MW = 7.5 Sonora, Mexico earthquake

<p>Electronic supplement to &quot;Structural configuration of the Otates fault (southern Basin-and-Range Province) and its rupture in the 3 May 1887 MW = 7.5 Sonora, Mexico earthquake&quot;&nbsp;(Seismological Society of America Bulletin, v. 98, no. 6, p. 2879-2893, 2008) with color-coded elevation model, satellite image of major Basin andRange normal faults in the study area, color version of geologic map, and additional photographs.</p> <p>High-resolution files of these figures are also available without restriction from&nbsp;</p> <p>http://www.seismosoc.org/Publications/BSSA_html/bssa_98-6/2008129-esupp/</p>

opencc-by-4.0Dec 2008View details →
zenodo36/100

SeisSol model setup of the Kaikōura's dynamic rupture model of Ulrich et al.

<p>All data required to run the dynamic rupture model of the Kaikōura earthquake presented in Ulrich, T., Gabriel, A. A., Ampuero, J. P., &amp; Xu, W. (2018). Dynamic viability of the 2016 Mw 7.8 Kaikōura earthquake cascade on weak crustal faults. A detailed readme file summarizing the data and data formats is also provided.</p>

opencc-by-4.0Jan 2019View details →
zenodo36/100

Dataset for "Dissecting abdominal aortic aneurysm in Ang II-infused mice: suprarenal branch ruptures and apparent luminal dilatation"

<p>This dataset contains histology, synchrotron and ultrasound data for the manuscript &quot;Dissecting abdominal aortic aneurysm<br> in Ang II-infused mice: suprarenal branch ruptures and apparent luminal dilatation&quot;, published in Cardiovascular Research in 2014.</p> <p>Histology data are zipped and to be opened using the Olympus-software OlyVIA, or with the BIOP-tool called VSI-reader, which is a plugin to the open-source software Fiji. Imaging data are saved in .mcs format and can be opened with the commercial software Mimics (Materialise, Leuven, Belgium). Filenames correspond to the mouse ID as it was used in the study.</p>

opencc-by-4.0Dec 2018View details →
zenodo36/100

SeisSol dynamic rupture model setup of the Mw 7.5 Palu earthquake scenario published in Ulrich et al. (2019)

<p>All data required to run the dynamic rupture model of the Palu earthquake presented in:</p> <p>Ulrich, T., Vater, S., Madden, E. H., Behrens, J., van Dinther, Y., van Zelst, I., Fielding, E. J., Liang, C. &amp; Gabriel, A. A. (2019). Coupled, Physics-based Modeling Reveals Earthquake Displacements are Critical to the 2018 Palu, Sulawesi Tsunami.&nbsp;doi: 10.31223/osf.io/3bwqa.</p> <p>A detailed readme file summarizing the data and data formats is also provided.</p>

opencc-by-4.0May 2019View details →
zenodo36/100

Data - Medial gastrocnemius muscle remodeling correlates with reduced plantar flexor kinetics fourteen weeks following Achilles tendon rupture

<p>ultrasound images and biodex data published used in analysis.</p> <p>study timeline:</p> <p>s1 - week 0</p> <p>s2 - week 2</p> <p>s3 - week 4</p> <p>s4 - week 6</p> <p>s5 - week 10</p> <p>s6 - week 14</p>

opencc-by-4.0Jul 2019View details →
zenodo36/100

In-vivo video microscopy of the rupturing process of thin blood vessels in transparent fish during contact with a blunt indenter

<p>To clarify the mechanism of bruise injuries caused by blunt impact, in vivo microscopy was performed. A flat ended indenter made of transparent acrylic was loaded onto the lateral side of the tail region of anesthetized fish. The process of the rupture of thin blood vessels was recorded in two specimens.</p> <p>This data set includes two types of files; (1) mp4 files of the in vivo microscopy; (2) pdf files to explain the mp4 files.</p> <p><span>The mp4 files are the original data of &ldquo;Fujikawa, T., Yamada, Y. In vivo video microscopy of the rupturing process of thin blood vessels to clarify the mechanism of bruising caused by blunt impact: an animal study. BioMed Eng OnLine 23, 94 (2024). https://doi.org/10.1186/s12938-024-01284-2.&rdquo;</span></p>

opencc-by-4.0Jul 2023View details →

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