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488 results for “Rupture”
SeisSol model setup input files and supplement videos for the 3D dynamic rupture models of Wirp et al. 2024
<p>Data required to run the dynamic rupture models presented in Wirp, S. A., Gabriel, A.-A., Ulrich, T., Lorito, S. (2024). The README.txt file contains detailed information about the data and data format.</p>
Text-fig. 7. Lusitanispermum choffatii gen. et sp. nov. seeds from the Early Cretaceous Famalicão locality (sample 025), Portugal; Synchrotron radiation X-ray tomographic microscopy (SRXTM, volume renderings). a) Holotype; seed in lateral view showing seed shape; note that the seed is broken near the lower surface of the hilum (S174345). b) Oblique apical view of micropylar-hilar region of holotype showing slightly ruptured micropylar slit (mi) in the outer integument and two bulging and abraded areas (arrow heads) close to hilum. c) Seed in oblique lateral-raphal view showing the two bulging structures (arrow heads) immediately adjacent to the lower edge of the hilum (S174472). d) Tangential, longitudinal cut (cut at yz0131) through the seed coat of seed in (7c) showing the undulate anticlinal cell walls of the exotesta cells that are thickest towards the outside and thinner towards the inside. Scale bars = 500 µm (a–c); 250 µm (d). in Extinct Taxa Of Exotestal Seeds Close To Austrobaileyales And Nymphaeales From The Early Cretaceous Of Portugal
Text-fig. 7. Lusitanispermum choffatii gen. et sp. nov. seeds from the Early Cretaceous Famalicão locality (sample 025), Portugal; Synchrotron radiation X-ray tomographic microscopy (SRXTM, volume renderings). a) Holotype; seed in lateral view showing seed shape; note that the seed is broken near the lower surface of the hilum (S174345). b) Oblique apical view of micropylar-hilar region of holotype showing slightly ruptured micropylar slit (mi) in the outer integument and two bulging and abraded areas (arrow heads) close to hilum. c) Seed in oblique lateral-raphal view showing the two bulging structures (arrow heads) immediately adjacent to the lower edge of the hilum (S174472). d) Tangential, longitudinal cut (cut at yz0131) through the seed coat of seed in (7c) showing the undulate anticlinal cell walls of the exotesta cells that are thickest towards the outside and thinner towards the inside. Scale bars = 500 µm (a–c); 250 µm (d).
2008 Nura earthquake surface rupture slip vector documentation
<p>This online data holds information related to the surface rupture resulting from the 2008 Nura earthquake in south Kyrgyzstan. The primary dataset is a Google Earth KMZ file with GPS-locations where slip vector measurements were taken along the rupture. A downloadable ZIP file accompanies the KMZ, containing photographs linked to each data point. Both files should be stored in one folder for proper linkage. In addition, a text file is available with all measurements and associated information. Five videos obtained with the drone are available to illustrate the surface rupture zones and geological overview in the Nura settlement surroundings. The entire data was gathered in 2018. </p> <p>Raster-files of high-resolution digital surface models of the surface rupture can be found on opentopography <a href="https://doi.org/10.5069/G9ZW1J4C" target="_blank" rel="noreferrer noopener">https://doi.org/10.5069/G9ZW1J4C</a></p> <p>The data presented in this repository was initially disseminated in a dissertation by Magda Patyniak. This project is part of the CaTeNA-project within the Client II program of and funded by the Federal Ministry of Education and Research (BMBF; Sub-project grant 03G0878E to Manfred Strecker).</p>
2002 and 2022 fault ruptures along the Timpe faults system (Mt. Etna)
<p>This dataset includes two shape files with ground ruptures observed on Mt. Etna in 2002 and 2022, in particular:</p> <ul> <li>the surface faulting, along the Santa Venerina, San Giovanni Bosco, Guzzi, and Scillichenti Faults accompanying the October 29 2002 earthquakes;</li> <li>the surface faulting along the creeping Scalo Pennisi (SCA) Fault observed on 29 October 2002 and 8 February 2022;</li> </ul> <p>Each shape file is associated with a database that contains information on: strike, length (m), heave (i.e., horizontal displacement in cm), throw (i.e., vertical displacement in cm), net slip displacement (cm), slip trend and plunge from certain piercing points.</p> <p>The dataset is associated with the paper: <em>"Aseismic creep and gravitational sliding on the lower eastern flank of Mt. Etna: insights from the 2002 and 2022 fault rupture events between Santa Venerina and Santa Tecla" </em>by G. Tringali, Bella, D., Livio F., Ferrario M. F., Groppelli G., Pettinato R., Michetti A. M.</p> <p> </p>
A Mixed-Flux-Based Nodal Discontinuous Galerkin Method for 3D Dynamic Rupture Modeling
<p>This repository contains data produced by a mixed-flux-based discontinuous Galerkin method for 3D dynamic rupture modeling, using the software DRDG3D (<a href="https://github.com/wqseis/drdg3d">https://github.com/wqseis/drdg3d</a>). Input scripts for the SCEC/USGS dynamic rupture benchmark validation problems (<a href="https://strike.scec.org/cvws">https://strike.scec.org/cvws</a>) and other cases are hosted on DRDG3D's GitHub page. The preprint is published at ESS Open Archive (DOI: <a href="http://doi.org/10.1002/essoar.10512657.1">10.1002/essoar.10512657.1</a>).</p>
Spreadsheet containing information on earthquakes that DID / DID NOT rupture the surface
<p>Spreadsheet containing information on earthquakes that DID / DID NOT rupture the surface</p> <p>Data are extracted from the ISC-GEM catalogue. Fields include:</p> <p>N.: identificative number, progressive</p> <p>Event ID: identificative number, from the ISC-GEM catalogue</p> <p>Date: format YYYY-MM-DD, from the ISC-GEM catalogue</p> <p>Lat: latitude of the epicenter, in decimal degrees</p> <p>Lon: longitude of the epicenter, in decimal degrees</p> <p>Depth, Depth unc and Depth quality: information retrieved from the ISC-GEM catalogue</p> <p>Mw, Mw unc and Mw quality: moment magnitude; information retrieved from the ISC-GEM catalogue</p> <p>Str, Dip, Rake: strike, dip and rake for the 2 nodal planes; information retrieved from the ISC-GEM catalogue</p> <p>Fault kin: earthquake mechanism, categorized as reverse, strike-slip, normal, transpressive, transtensive</p> <p>Surface faulting: categorized as YES, NO, no info, debated faulting</p> <p>SRL (surface rupture length in km); MD (max displacement in m); AD (average displacement in m)</p> <p>Reference: literature used to compile the dataset; full list is available in the .pdf file related to this document</p> <p> </p> <p>A poster has been presented at the PATA Days 2023 in France, file available at:</p> <p><a href="https://www.researchgate.net/publication/363739186_LIKELIHOOD_OF_PRIMARY_SURFACE_FAULTING_A_SEQUEL">https://www.researchgate.net/publication/363739186_LIKELIHOOD_OF_PRIMARY_SURFACE_FAULTING_A_SEQUEL</a></p>
Supplementary materials for: Multiple ruptures on the North Sofia fault at Gorni Bogrov from scarp profile and shallow geophysics
<p>The data set contains resistivity data of two profiles that were measured at Gorno Bogrov site in the Sofia basin in Bulgaria. The resistivity survey was performed to study the North Sofia fault.</p> <p>The resistivity data in files r1ohm.tx and r2ohm.txt should be inverted using the BERT software (http://resistivity.net/) with configuration files r1cfg.txt and r2icfg.txt, respectively. The file bog2.txt contains fault coordinates for constraining the inversion mesh of the shorter profile (files r2ohm.txt, r2icfg.txt).</p> <p>The data set was collected within the project Assessment of Earthquake Ground Motion Amplification in the Sofia Basin (<a href="http://sofiabasin.atwebpages.com/">http://sofiabasin.atwebpages.com/</a>), funded by the Bulgarian National Science Fund, contract number KP-06-N64/1 from 15.12.2022.</p>
Data repository for Pore Pressure Drop during Dynamic Rupture and Conditions for Dilatancy Hardening
<p>Simulation data to accompany publication Pore pressure drop during dynamic rupture and conditions for dilatancy hardening, submitted to Journal of Geophysical Research: Solid Earth. See Readme.txt for content of data files. The data were generated by 'GrandFrix' software and postprocessed by scripts written MATLAB – see Related identifiers.</p>
26 December 2018 surface ruptures along the eastern flank of Mt. Etna
<p>This dataset includes two shape files with ground breaks observed on Mt. Etna after the 26 December 2018 earthquake and aseismic creep event, in particular:</p> <ul> <li>the surface faulting, along the Fleri, Fiandaca, Aci Catena and Aci Platani faults;</li> <li>the ground breaks related to slope instabilities;</li> </ul> <p>The shape files have a database with informations on: strike, length (m), heave (i.e., horizontal displacement in cm), throw (i.e., vertical displacement in cm), strike-slip (cm), net slip displacement (cm), kinematics, slip trend and plunge from certain piercing points.</p> <p>The dataset is an updated and an upgrade of the one associated with the paper: <em>"Fault rupture and aseismic creep accompanying the December 26, 2018, Mw 4.9 Fleri earthquake (Mt. Etna, Italy): Factors affecting the surface faulting in a volcano-tectonic environment" </em>by G. Tringali, Bella, D., Livio F., Ferrario M. F., Groppelli G., Blumetti A.M., Di Manna P., Vittori T., Guerrieri L., Porfido S., Boso D., Pettinato R., Paradiso G., Michetti A.M. (<a href="https://doi.org/10.1016/j.quaint.2021.12.019">https://doi.org/10.1016/j.quaint.2021.12.019</a>).</p>
A role for myosin II cluster and membrane energy in cortex rupture for Dictyostelium discoideum cells
Open the record for dataset details and reuse information.
Analysis of copy number variation in dogs implicates genomic structural variation in the development of anterior cruciate ligament rupture
Open the record for dataset details and reuse information.
DATA SET FOR: Active faulting, submarine surface rupture and seismic migration along the Liquiñe-Ofqui fault system, Patagonian Andes
<p>Data description: These data corresponde to high-resolution bathymetry and seismic reflection profiles obtained in the inner fjord west of Puerto Aysén (between 73.13°- 72.68°W and 45.32°-45.47°S; Figs. 1 and 2). The data set was obtained during a geophysical study as part of the DETSUFA project (Deslizamientos Tsunamigénicos en el Fiordo de Aysén; Lastras et al., 2013), which took place between March 4th and 17th, 2013, aboard the R/V BIO Hésperides.<br> <br> KONGSBERG SIMRAD multibeam EM-1002S was used to obtain bathymetric data, and it works with 111 beams at a 96 kHz sonar frequency and with a maximum ping rate of >10 Hz. Equidistant mode was used for swath bathymetry acquisition. This array maximized the number of beams facilitating data acquisition and obtaining a homogenized final grid with improved resolution, with tracks separated every 150 m. The swath thickness was the same regardless of width, generating a 50% overlap between each track, with the exception of areas located near the coast. Expendable Bathythermograph (XBT) probes were used at specific sites to measure changes in water sound velocity due to eventual changes in fresh water circulation, tides, and sediment.<br> <br> Seismic reflection data were acquired using an array of two BOLT air guns (165 and 175 inches3), which were towed behind the vessel stern. The configuration used in the seismic sources was 2,000 psi, a depth of 3 m for the gun, with a firing rate of 15 m over the seafloor. A 100 m long mini-streamer with a 25 m active section, corresponding to one single channel, recovered the shots. The seismic data were recorded by using the DELPH SEISMICPLUS system with a recording length of 4.0 s and a preamplifier gain of 8 Hz. The raw seismic data were processed aboard the SMT Kingdom Suite, including the navigation and standard processes of electrical noise removing (50 Hz filter), gain amplifier and bandpass filtering, to improve data visualization. Postprocessing included the migration of the sea bottom diffractions and the muting of the water column performed in Seismic-Unix.</p> <p>Files:</p> <p>Raw Seismic reflection data for lines 05, 06 and 07 (SU & SEG files)</p> <p>Masked Seismic profiles for lines 05, 06 and 07 (SU, PDF & PS files)</p> <p>Bathymetry of inner and outer Aysén Fjord (ASCII file)</p>
2020 Cascadia rupture models
<p>Synthetic rupture scenarios for 32,500 ruptures o the Cascadia subduction zone. This dataset accompanies the paper "The January 26th, 1700 Cascadia Earthquake as Part of an Event Sequence".</p> <p>There are 5 subfolders for ruptures generated assuming different background mean models. The .log file contains details on each rupture, the .rupt file contains the rupture definitions and the .xy file is used for plotting in GMT. The columns fo the .rupt file are as follows:</p> <ul> <li>Subfault number</li> <li>Longitude of subfault centroid</li> <li>Latitude of subfault centroid</li> <li>Depth of subfault centroid (km)</li> <li>Strike of subfault (degs)</li> <li>Dip of subfault (degs)</li> <li>Dummy variable</li> <li>Rise time (s)</li> <li>Slip in the rake = 0 direction (m)</li> <li>Slip in the rake = 90 direction (m)</li> <li>Length of subfault (m)</li> <li>Width of subfault (m)</li> <li>Rupture onset time (s)</li> <li>Rigidity at depth of subfault centroid (Pa)</li> </ul> <p> </p>
LIST OF RECENT EARTHQUAKES THAT POSSIBLY HAD SURFACE RUPTURE
<p>The Excel spreadsheet and its accompanying text file list all the shallow (<35 km) M6+ earthquakes that have occurred on-land in the period 2000-2016. These are of a size and type of earthquake that may have produced surface faulting. So in updating the SURE database, we need to ensure that we know whether each of these 134 earthquakes produced surface rupture, and how much. At this point it looks like there are published papers about surface faulting for 20 of these earthquakes. For the rest, we don't know if there was surface rupture or not. I suggest we ask for volunteers from the countries that contain these 114 undocumented earthquakes, and ask them if surface rupture was looked for, and if so, if it was found and what parameters were measured. These volunteers would come from the SURFACE project, or be new paleoseismologists who would like to become involved.</p>
Template for implementation of the Surface Rupture Database (SURE)
<p>The structure of the "surface rupture database" (SURE) has been discussed during a workshop in Paris. Please find details at www.earthquakegeology.com/materials/projects/1620R-report.pdf </p> <p> </p>
Quantifying the erasure of earthquake surface ruptures from desert landscapes: Implications for seismic hazard assessment
<p><strong>Original Landscapes</strong></p> <p>DEMs of ~120x140m landscapes clipped from:</p> <p>R1-10 = 2019 M7.1 Ridgecrest earthquake, 2019 lidar (Hudnut et al., 2020), and </p> <p>E1-10 = 2010 M7.2 El Mayor-Cucapah earthquake, 2010 lidar (OpenTopography, 2010).</p> <p>Example: "E5.asc"</p> <p> </p> <p><strong>Degraded Landscapes</strong></p> <p>Linearly diffused using <em>Landlab </em>(Hobley et al., 2017; Barnhart et al., 2020) at timesteps (100, 1000, 5000, 10000 yr) using a <em>k</em> of 1 m^2/kyr.</p> <p>Example: "e5_1000_001_eroded.asc"</p> <p> </p> <p><strong>Mapped Faults Shapefiles </strong>- E1_10_shps & R1_10_shps</p> <p>Faults mapped on each degraded landscape using a systematic mapping process (Scott et al., 2023; Adam, 2023)</p> <p> </p> <p><strong>Ridgecrest DEM</strong> - rc_7_1_0424_utm.tif</p> <p>0.014 m/pix DEM of a portion of the 2019 M7.1 Ridgecrest earthquake rupture, from 6 April 2024. Created from Structure from Motion using drone images. </p> <p> </p> <p><strong>Degradation and analysis python code</strong> - landscape_evolution_earthquake_ruptures-main.zip</p> <p>A set of scripts to simulate the effect of surface processes on surface ruptures and quantify the information loss associated with landscape evolution over time. Includes options to simulate surface processes with linear and non-linear diffusion, implemented using open-access code landlab.</p> <p> </p> <p><strong>References</strong></p> <p>Adam, R. (2023). Evaluation of remote mapping of active fault traces. Arizona State University.</p> <p>Barnhart, K.R., Hutton, E.W.H., Tucker, G.E., Gasparini, NM., Istanbulluoglu, E., Hobley, D.E.J., Lyons, N.J., Mouchene, M., Nudurupati, S.S., Adams, J.M., Bandarogoda, C., 2020, Short communication: Landlab v2.0: A software package for Earth surface dynamics: Earth Surface Dynamics Discussions, doi: 10.5194/esurf-2020-12.</p> <p>Hobley, D.E.J., Adams, J.M., Nudurupati, S.S., Hutton, E.W.H. Gasparini, N.M., Istanbulluoglu, E., and Tucker, G.E., 2017, Creative computing with Landlab: an open-source toolkit for building, coupling, and exploring two-dimensional numerical models of Earth-surface dynamics: Earth Surface Dynamics, v. 5, n. 1, p. 21-46, doi: 10.5194/esurf-5-21-2017.</p> <p>Hudnut, K.W., B. Brooks, K. Scharer, J.L. Hernandez, T.E. Dawson, M.E. Oskin, R. Arrowsmith, C.A. Goulet, K. Blake, M.L. Boggs, S. Bork, C.L. Glennie, J.C. Fernandez-Diaz, A. Singhania, D. Hauser, S. Sorhus (2020). 2019 Ridgecrest, CA Post-Earthquake Lidar Collection. National Center for Airborne Laser Mapping (NCALM). Distributed by OpenTopography. https://doi.org/10.5069/G9W0942Z.. Accessed: 2024-11-25 </p> <p>Opentopography; El Mayor-Cucapah Earthquake (4 April 2010) Rupture LiDAR Scan. Distributed by OpenTopography. https://doi.org/10.5069/G9TD9V7D . Accessed: 2024-11-25</p> <p>Scott, C., Adam, R., Arrowsmith, R., Madugo, C., Powell, J., Ford, J., Gray, B., Koehler, R., Thompson, S., Sarmiento, A., Dawson, T., Kottke, A., Young, E., Williams, A., Kozaci, O., Oskin, M., Burgette, R., Streig, A., Seitz, G., … Ingersoll, S. (2023). Evaluating how well active fault mapping predicts earthquake surface-rupture locations. Geosphere. https://doi.org/10.1130/GES02611.1</p>
Identification of genetic variants associated with anterior cruciate ligament rupture and AKC standard coat color in the Labrador Retriever
<p>Canine anterior cruciate ligament (ACL) rupture is a common complex disease. Prevalence of ACL rupture is breed-dependent. In an epidemiological study, yellow coat color was associated with increased risk of ACL rupture in the Labrador Retriever. ACL rupture risk variants may be linked to coat color through genetic selection or through linkage with coat color genes. To investigate these associations, Labrador Retrievers were phenotyped as ACL rupture cases or controls and for coat color and were single nucleotide polymorphism (SNP) genotyped. After filtering, ~697K SNPs were analyzed using GEMMA and mvBIMBAM for multivariate association. Functional annotation clustering analysis with DAVID was performed on candidate genes. A large 8Mb region on chromosome 5 that included <em>ACSF3</em>, as well as 32 additional SNPs, met genome-wide significance at <em>P</em><6.07E-7 or Log<sub>10</sub>(BF) = 3.0 for GEMMA and mvBIMBAM, respectively. On chromosome 23, SNPs were located within or near <em>PCCB</em> and <em>MSL2</em>. On chromosome 30, a SNP was located within <em>IGDCC3</em>. SNPs associated with coat color were also located within <em>ADAM9</em>,<em> FAM109B</em>,<em> SULT1C4</em>,<em>RTDR1</em>,<em> BCR</em>, and <em>RGS7</em>. <em>DZIP1L</em> was associated with ACL rupture. Several significant SNPs on chromosomes 2, 3, 7, 24, and 26 were located within uncharacterized regions or long non-coding RNA sequences. This study validates associations with the previous ACL rupture candidate genes <em>ACSF3</em> and <em>DZIP1L</em> and identifies novel candidate genes. These variants could act as targets for treatment or as factors in disease prediction modeling. The study highlighted the importance of regulatory SNPs in the disease, as several significant SNPs were located within non-coding regions.</p>
Coseismic frictional heating with concomitant hydrothermal fluid circulation revealed by rock magnetic properties of fault rocks from the rupture of the 2008 Wenchuan earthquake, China
<p>This repository contains the rock magnetic data associated with the manuscript entitled "Coseismic frictional heating with concomitant hydrothermal fluid circulation revealed by rock magnetic properties of fault rocks from the rupture of the 2008 Wenchuan earthquake, China" by Yan et al. published in <i>Geochemistry, Geophysics, Geosystems, </i>24, e2023GC011223. https://doi.org/10.1029/2023GC011223</p>
Data repository for: Frictional weakening leads to unconventional singularities during dynamic rupture propagation
<p>Laboratory data to accompany publication <span>Frictional weakening leads to unconventional singularities during dynamic rupture propagation</span>, submitted to Earth and Planetary Science Letters.</p> <p>For any further queries please contact federica.paglialunga@epfl.ch</p>
A decade of short-period earthquake rupture histories from multi-array back-projection
<p>Data Set S1: *.bp files containing the short-period earthquake rupture patterns, energy radiated maps, and source time functions.</p> <p>Data Set S2: Earthquake source information and rupture parameter estimates in machine-readable format (*.csv file) based on visually determined rupture end times.</p> <p>Data Set S3: Rupture parameter estimates in machine-readable format (*.csv file) based on automatic rupture end times.</p>
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Allen Brain Atlas
Allen Brain Atlas is an Allen Institute collection of brain map atlases, datasets, APIs, and analysis tools covering mouse, human, and non-human primate brain resources.
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DANDI Archive for NWB datasets
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The International Brain Laboratory public data releases expose standardized mouse decision-making experiments, including Neuropixels recordings, widefield calcium imaging, behavior, and session metadata accessed through the ONE API.
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