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206 results for “subduction”
Mechanical data of rotary shear fluid pressurised experiments for the manuscript: "Fluid pressurisation and earthquake propagation in the Hikurangi subduction zone"
<p>Mechanical data of rotary shear fluid pressurised experiments.</p> <p>Tab-delimited file with calibrated measurements of:</p> <ul> <li>Time (milliseconds)</li> <li>Normal stress: Normal (MPa) </li> <li>Fault displacement: Slip (mm)</li> <li>Fault velocity: Velocity (mm/s)</li> <li>Shear stress: Shearstress (MPa)</li> <li>Downstream Pore Pressure: Pressure_ds (MPa)</li> <li>Confining Pressure: Pressure_conf (MPa)</li> <li>Upstream pore pressure: Pressure_us (MPa)</li> <li>Temperature of the upstream boundary of the gouge layer: Temperature_us (°C)</li> <li>Thickness of the gouge layer: Thickness (mm).</li> </ul>
Dataset Publication for "A Comprehensive Stress Drop Map from Trench to Depth in the Northern Chilean Subduction Zone"
<p><strong>Abstract</strong>: Stress drop catalog data publication supplement for "A Comprehensive Stress Drop Map from Trench to Depth in the Northern Chilean Subduction Zone" (Folesky, J., Pennington, CN., Kummerow J., Hofman LR. (JGR: Solid Earth, 2023) <a href="https://doi.org/10.1029/2023JB027549">https://doi.org/10.1029/2023JB027549</a>), obtained from wave form analysis using the spectral decomposition technique. Time duration is 2007 to 2021. Seismic events were taken from the IPOC catalog (Sippl, C., Schurr, B., Münchmeyer, J., Barrientos, S., Oncken, O. (2023): Catalogue of Earthquake Hypocenters for Northern Chile from 2007-2021 using IPOC (plus auxiliary) seismic stations.<br><a title="Follow link" href="https://doi.org/10.5880/GFZ.4.1.2023.004" target="_blank" rel="nofollow noopener">https://doi.org/10.5880/GFZ.4.1.2023.004</a>). Wave forms were obtained from the EIDA/GEOPHONE web page (eida.gfz-potsdam.de/webdc3/ or geofon.gfz-potsdam.de/waveform/)</p> <p><strong>File descriptions</strong>: table columns <br>ID, cls, Lon, Lat, Depth, Magntiude, vssource, fc1, fcbound1, fcbound2, sd<br>------------------<br>explanation<br>ID : origin time<br>cls : event class<br>Lon : longitude <br>Lat : latitude<br>Depth : depth in km<br>Magnitude : magnitude (MA)<br>vssource. : s- wave velocity at the event location<br>fc1. : corner frequency in Hz<br>fcbound1 : lower bound for fc1 from 5% variance reduction test in Hz<br>fcbound2. : upper bound for fc2 from 5% variance reduction test in Hz<br>sd : stress drop estimate in MPa</p>
Seismic Azimuthal Anisotropy Model Beneath the Alaska Subduction Zone
<p>This dataset is supplementary to:</p> <p>Liu, C., Sheehan, A.F., Ritzwoller, M.H. (2024) (Under review).</p> <p>The uploaded file uses NetCDF4 format and contains isotropic Vsv and depth-dependent azimuthal anisotropy.</p> <p>File format:</p> <p><code>Longitude</code>, <code>Latitude</code>, <code>Depth</code>, <code>Para</code></p> <ul> <li> <p>Dimensions:</p> <ul> <li><code>Longitude</code>: -164.2° to -142.8° with 0.8° interval.</li> <li><code>Latitude</code>: 53.6° to 65.6° with 0.4° interval.</li> <li><code>Depth</code>: 10 to 200 with 5 km interval</li> </ul> </li> <li>Model parameters:<br> <ul> <li><code>vsv</code>: isotropic shear wave velocity (km/s)</li> <li><code>unc_vsv</code>: uncertainty for isotropic shear wave velocity </li> <li><code>fa</code>: depth-dependent fast azimuth (deg)</li> <li><code>unc_vsv</code>: uncertainty for depth-dependent fast azimuth</li> <li><code>amp</code>: depth-dependent anisotropy amplitude (%)</li> <li><code>unc_amp</code>: uncertainty for depth-dependent anisotropy amplitude</li> </ul> </li> </ul> <p> </p>
Data from 666 earthquake/tsunami scenario simulations targeting Nankai subduction
<p><strong>Summary: </strong></p> <ul> <li>Data from 666 earthquake/tsunami scenario simulations targeting Nankai subduction</li> <li>Tsunami simulation solver: TUNAMI-N2</li> <li>Fault rupture model: Okada model(Okada, 1985)</li> <li>Each scenario data consists of 71 ASCII files containing the simulated wave sequences at the synthetic gauges </li> <li>Each single scenario is tagged as "Nankai-XYZE", where XYZW would be the number from <strong>0003</strong> to <strong>1470</strong>.</li> <li>Some of the synthetic gauges are located based on the real ocean gauge points (e.g., DONET2, NOPHAS) nearby Shikoku region, Japan.</li> </ul> <p> </p> <p><strong>Details of each file:</strong></p> <ul> <li><strong>wave_sequenses.tar.gz</strong>: A series of wave sequences (4-hour wave history-data, recorded every 5 seconds) at 71 synthetic gauges are provided in ascii type format. <br> Note that <strong>5.8GB additional storage would be required</strong> to fully unzip this archive file with the following command. <pre><code>tar xzvf wave_sequences.tar.gz</code></pre> <p>You can get all scenario data as follows:</p> <pre><code>wave_sequences ├ Nankai-0003 ├ Nankai-0004 ├… ├ Nankai-1467 └ Nankai-1470 </code></pre> <p>Each directory contains the 71 files, head with 'pntX_Y.asc',</p> <pre><code>Nankai-0003 ├ pnt1_01.asc ├ pnt1_02.asc ├... ├ pnt5_46.asc └ pnt5_47.asc</code></pre> <p>which contains the wave sequence data. The ASCII file, the time (minute) elapsed from the fault rupture is aligned in the left column, and the wave displacements \eta (meter) from the original surface location are in the right column.</p> </li> </ul> <ul> <li> <p><strong>quake_params.csv</strong>: The parameter used to generate 666 earthquake scenarios caused by the rupture of rectangular fault, by means of Okada model. (Okada 1985)</p> </li> </ul> <ul> <li><strong>synthetic_gauges.csv</strong>: The locations of 71 synthetic gauges. </li> </ul>
Global kinematics of tectonic plates and subduction zones since the late Paleozoic Era
<div>Global kinematics of tectonic plates and subduction zones since the late Paleozoic Era</div> <div> </div> <div>Alexander Young(1), Nicolas Flament(1), Kayla Maloney(2), Simon Williams(2), Kara Matthews(2), Sabin Zahirovic(2), Dietmar Müller(2,3)</div> <div> </div> <div>1. The University of Wollongong, NSW 2522, Australia </div> <div> </div> <div>2. EarthByte Group, School of Geosciences, The University of Sydney, NSW 2006, Australia</div> <div> </div> <div>3. Sydney Informatics Hub, The University of Sydney, NSW 2006, Australia </div> <div> </div> <div>Contact: ajy321@uowmail.edu.au</div> <div> </div> <div> </div> <div>Supplementary Material</div> <div> </div> <div>We provide the digital plate model files (including rotations and geometries). These files allow for the visualisation and/or manipulation of the late Paleozoic to present-day (410-0 Ma) global plate motion model presented in this study. </div> <div> </div> <div>#########################################</div> <div>The digital plate model files are compatible with the open-source GPlates plate reconstruction software (<a href="https://www.gplates.org" target="_blank" rel="noopener">www.gplates.org</a>):</div> <div> </div> <div>(1) Rotations - Global rotation model that contains the reconstruction poles that describe the motions of the continents and oceans.</div> <div>- <strong>Global_250-0Ma_Young_et_al.rot</strong> (455 KB)</div> <div>-<strong> Global_410-250Ma_Young_et_al.rot</strong> (154 KB)</div> <div> </div> <div>(2) Plate polygons and boundary geometries - Topologically closed plate polygons are constructed from the intersection of ridges, transforms, subduction zones and other plate boundary geometries. These 'resolved topologies' are defined at 1 Myr intervals (410-0 Ma). The plate boundary geometries and plate polygons have been assigned plate reconstruction IDs to allow them to be reconstructed using the supplied rotation file.</div> <div>- <strong>Global_Mesozoic-Cenozoic_plate_bounds_Young_etal.gpml</strong> (36.5 MB)</div> <div>- <strong>Global_Paleozoic_plate_bounds_Young_etal.gpml</strong> (6.7 MB)</div> <div>- <strong>TopologyBuildingBlocks_Young_etal.gpml</strong> (2 MB) - this file is identical to Müller et al. (2016)</div> <div> </div> <div>(3) Coastlines - Geometries of the present-day coastlines.</div> <div>- <strong>Global_coastlines_Young_et_al_low_res.shp</strong> (1.2 MB including auxiliary files, datum-WGS 1984)</div> <div> </div> <div>(4) Static polygons (optional) - Includes ocean isochron and terrane polygon geometries.</div> <div>- <strong>GlobalPresentDay_SPP_Young_etal.shp</strong> (1.4 MB inc. auxillary files, datum-WGS 1984)</div> <div> </div> <div>(5) Continental polygons (optional) - Includes continental terrane polygon geometries and excludes oceanic lithosphere.</div> <div>- <strong>PresentDay_ContPolygons_Young_etal.shp</strong> (451 KB inc. auxillary files, datum-WGS 1984)</div> <div> </div> <div>GPlates: </div> <div>To view the model, load all files in GPlates (either drag and drop files onto the globe OR from the navigation bar at the top of the screen click File -> Open Feature Collection and select files). Both rotation files (1) and each of the three plate geometry files (2) need to be loaded for the model to work properly. It is recommended that coastlines (3) are loaded to see how the continents move, however only one coastline file is necessary (.gpml or .shp). The static polygons (4) and continental polygons (5) are optional. </div> <div> </div> <div>The two rotation files need to be 'connected' in order for the model to run continuously from 410 to 0 Ma. In the GPlates 'Layers' window (opened from the main navigation bar, click 'Window' -> 'Show Layers') the rotation files will be highlighted yellow, yet only one will have a yellow tick next to it to signify it is being used. Click the small black triangle to the left the ticked rotation file. Under 'Inputs' -> 'Reconstruction features' click 'Add new connection' and then select the other rotation file from the list of files that will appear. This will ensure that both rotation files are active. </div> <div> </div> <div>Finally, it is recommended to experiment with geometry visibility in order to make the globe less cluttered. For instance, from the navigation bar click View -> Geometry Visibility and untick 'Show Line Geometries'. Alternatively, files can be toggled on and off using the tick boxes in the Layers window. For more information about using GPlates, a set of user tutorials can be accessed from the GPlates website - http://www.gplates.org/docs.html.</div> <div> </div> <div> </div> <div>#########################################</div> <div>MODEL REFERENCING:</div> <div>When using our model, in addition to citing this publication, please consider citing the studies of Domeier and Torsvik (2014), Matthews et al. (2016) and Müller et al. (2016) which served as the basis for this model in the late Paleozoic and Mesozoic-Cenozoic, respectively, and citing any other study that describes refinements to the plate reconstructions in your region of interest as appropriate. </div> <div> </div> <div>- Domeier, M., & Torsvik, T. H. (2014). Plate tectonics in the late Paleozoic. Geoscience Frontiers, 5(3), 303-350. DOI: <a href="https://doi.org/10.1016/j.gsf.2014.01.002" target="_blank" rel="noopener">10.1016/j.gsf.2014.01.002</a></div> <div>- Müller, R. D., Seton, M., Zahirovic, S., Williams, S. E., Matthews, K. J., Wright, N. M., Shephard, G. E., Maloney, K., Barnett-Moore, N., Hosseinpour, M., Bower, D. J., & Cannon, J. (2016). Ocean Basin Evolution and Global-Scale Plate Reorganization Events Since Pangea Breakup. Annual Review of Earth and Planetary Sciences, 44(1). DOI: <a href="https://doi.org/10.1146/annurev-earth-060115-012211" target="_blank" rel="noopener">10.1146/annurev-earth-060115-012211</a></div> <div>-Matthews, K. J., Maloney, K. T., Zahirovic, S., Williams, S. E., Seton, M., & Mueller, R. D. (2016). Global plate boundary evolution and kinematics since the late Paleozoic. Global and Planetary Change, 146, 226-250.</div> <div>DOI: <a href="https://doi.org/10.1016/j.gloplacha.2016.10.002" target="_blank" rel="noopener">10.1016/j.gloplacha.2016.10.002</a></div>
Data from: Dating and morpho-stratigraphy of uplifted marine terraces in the Makran subduction zone (Iran)
<p>This data comes from the study of marine terraces from the Iranian Makran. This second version contains .zip compressed files instead of .rar .<br> A_files are seven terrace maps of the region of Jask, Tang, Gurdim, Konarak, Chabahar-Ramin, Lipar and Pasabander.<br> B_file are results of Radiocarbon and 230Th/U dating of mollusk shells from the marine deposits above the terraces.<br> C_file are results of Optically Stimulated Luminescence dating (OSL) of said deposits.<br> D_files are field pictures.<br> The data is published in support for the paper mentioned in the title (submitted to Earth Surface Dynamics).</p> <p>Brief description:<br> Terrace maps are accompanied with a datamodel excel file explaining the different GIS layers.<br> The maps are provided in both .KMZ files (for Google Earth) and Shapefiles</p> <p>Radiometric (i.e. both Radiocarbon and 230Th/U) analytical details are provided, together with XRD analysis of the Aragonitic shells and some SEM pictures of both Aragonitic and Calcitic shells. Method details are in the paper.</p> <p>OSL results are provided with the analytical details, such as: Environmental dose parameters, OSL raw measurements (out of the machine), OSL Histograms, Dose-Recovery tests and Fading test results. Method details are in the paper.</p> <p>Additional field pictures are provided with their legends (.txt file) and geolocalisation (.kmz file).</p>
Data from 1564 earthquake/tsunami scenario simulations targeting the Nankai Trough subduction zone
<p><strong>Summary:</strong></p> <ul> <li>Data from 1564 earthquake/tsunami scenario simulations targeting the Nankai Trough subduction zone</li> <li>Tsunami simulation solver: TUNAMI-N2</li> <li>Fault rupture model: Okada model (Okada, 1985)</li> <li>Each scenario data comprises 247 ASCII files storing the simulated wave sequences at synthetic gauges.</li> <li>Every single scenario is tagged as "JNan_X.X_YYY", where X.X indicates the magnitude and YYY is a serial number.</li> <li>Some synthetic gauges are in identical locations to actual ocean gauges (e.g., DONET2, NOWPHAS) near Shikoku, Japan.</li> </ul> <p><strong>Details of each file:</strong></p> <ul> <li><strong>data.tar.gz:</strong> A series of wave sequences (6-hour wave historical data, recorded every 5 seconds) at the 247 virtual gauges. Note that 52 GB of additional storage would be required to fully unzip this archive file with the following command. <pre><code>tar xzvf data.tar.gz</code></pre> <p>The unzipped directory contains all scenario data as follows:</p> <pre><code>data ├── JNan_7.6_001 ├── JNan_7.6_002 ├── JNan_7.6_003 ├── ├── ├── JNan_8.8_326 ├── JNan_8.8_327 └── JNan_8.8_328</code></pre> <p>Each directory contains 247 files named 'pntX_YY.asc'.</p> <pre><code>JNan_X.X_YYY ├── pnt1_01.asc ├── pnt1_02.asc ├── pnt1_03.asc ├── ├── ├── pnt5_46.asc ├── pnt5_47.asc └── pnt5_48.asc</code></pre> <p>In each ASCII file, the time (minute) elapsed from the fault rupture is aligned in the left column, and the wave displacements (meter) from the original sea level are in the right column.</p> </li> <li> <p><strong>quake_params.csv:</strong> The parameter used to generate 1564 earthquake scenarios caused by the rupture of rectangular fault, by means of the Okada model (Okada 1985)</p> </li> <li> <p><strong>synthetic_gauges.csv:</strong> The locations of the 247 synthetic gauges</p> </li> </ul>
Topographic fingerprint of deep mantle subduction
<p>This dataset contains the extracted velocities (Vt, Vconv), the time, as well as the surface topographic signals (Hsurf, Hdyn) of the models presented in the paper.</p>
Where does subduction initiate and cease? A global scale perspective (Supplementary material)
<p>Supplementary material for Where does subduction initiate and cease? A global scale perspective</p>
Intermediate depth earthquakes at the Hikurangi subduction zone, New Zealand
<p>This dataset contains a catalogue of intermediate depth earthquakes in the Hikurangi Subduction Zone, New Zealand, as well as computed focal mechanisms.</p> <p>If you use this dataset please cite the following paper:</p> <p>Mark, O.K., Illsley‐Kemp, F., Townend, J. and Barker, S.J., 2024. Evidence From Intermediate‐Depth Earthquakes of Slab‐Derived Fluids Beneath the Taupō Volcanic Zone. <em>Journal of Geophysical Research: Solid Earth</em>, <em>129</em>(5), p.e2023JB028586.</p>
Data, multiscale dataset and supplementary information for 'Pulsed fluid release from subducting slabs caused by a scale-invariant dehydration process'
<p>This repository contains the analytical Supplementary Information, the data, the multiscale dataset and the codes used to construct the dataset and plot figures used in the manuscript 'Pulsed fluid release from subducting slabs caused by a scale-invariant dehydration process' (accepted in Earth and Planetary Science Letters). </p> <p> </p> <p> </p>
Global Hydrogen Production during high-pressure Serpentinisation of Subducting Slabs—Dataset
<p>Data-set and code for recreating results of:</p> <p><strong>Global Hydrogen Production during high-pressure Serpentinisation of Subducting Slabs </strong></p> <p>A manuscript submitted to G-cubed.</p> <p> </p>
Data file for: Electrical imaging for the subduction channel north of Mount Everest
<p>The magnetotellurics data were used to study the the subduction channel north of Mount Everest, conducted by Institute of Geophysical and Geochemical Exploration, Chinese Academy of Geological Sciences. The data file of zf.dat was generated by the Matlab code EM3DVP.</p> <p>You are recommended to refer to the Kelbert et al., 2014 paper: https://doi.org/10.1016/j.cageo.2014.01.010 for a brief understanding of the data file formats.</p>
Subduction zone initiation (SZI) Database
<p>The <strong>Subduction zone initiation (SZI) Database</strong> is a <em>cross-disciplinary</em> and <em>community-driven</em> approach to gain an improved understanding of subduction zone initiation (SZI) and overcome the key long-standing questions of the Earth Sciences of how, when and where it happens on the Earth.</p> <p>The interdisciplinary database features more than a dozen documented SZI events that occurred during the last hundred million years. The SZI Database and its related online platform, <a href="http://www.szidatabase.org"><strong>www.szidatabase.</strong></a><strong><a href="http://www.szidatabase.org">org</a>,</strong> is an easily-accessible, fully transparent, expandable platform that contains relevant SZI data and analyses, and establishes a common language to sharpen discussion across the Earth Science community.</p> <p>Further details and the first novel scientific insights gained based on the database are presented in <a href="https://rdcu.be/b5ROu">Crameri et al. (2020, Nature Communications)</a>.</p>
List of VLFEs obtained in the paper "Influence of a subducted oceanic ridge on the distribution of shallow VLFEs in the Nankai Trough as revealed by moment tensor inversion and cluster analysis"
<p>List of VLFEs obtained in Toh et al., (2020, GRL).</p> <p>"Influence of a subducted oceanic ridge on the distribution of shallow VLFEs in the Nankai Trough as revealed by moment tensor inversion and cluster analysis" by Akiko Toh, Wan-Jou Chen, Nozomu Takeuchi, Douglas Dreger, Wu-Cheng Chi, and Satoshi Ide. </p> <p> </p>
Chilean Subduction Zone rupture scenarios and waveform data
<p>Chilean Subduction Zone kinematic rupture scenarios and waveform data for the submitted work <strong>Early warning for great earthquakes from characterization of crustal deformation patterns with deep learning (2020)</strong> by Lin et al.</p>
An introductory review of thermal structure of subduction zones: II & III
<p>This repository contains the output from a global suite of subduction zone models used in: "An introductory review of the thermal structure of subduction zones: II—numerical approach and validation", Wilson & van Keken, PEPS, 2023 and "An introductory review of the thermal structure of subduction zones: III—Comparison between models and observations", van Keken & Wilson, PEPS, 2023.</p> <p><strong>Directories & Files</strong></p> <p>The subdirectories of `vankeken_wilson_peps_2023.zip` are:</p> <ul> <li> <p><span>`</span><span>D80</span><span>`</span><span>: a reproduction of the "D80" Syracuse et al., PEPI, 2010 suite of subduction zones with a "dynamic" slab (Stokes equations solved </span><span>in the slab portion of the domain as in van Keken & Wilson, PEPS, 2023 and </span><span>`</span><span>D80new</span><span>`</span><span> below) and performed using Sepran</span></p> </li> <li> <p>`D80new`: a new global suite based on Syracuse et al., PEPI, 2010 but using a lower mantle potential temperature and an error function boundary condition and performed using both Sepran and TerraFERMA. Input files provided for TerraFERMA.</p> </li> <li> <p>`benchmark`: a new subduction benchmark performed using both Sepran and TerraFERMA. Input files provided for TerraFERMA.</p> </li> <li>`Figure_III_4_models`: the results used in Figure 4, Part III.</li> </ul> <p>Files include:</p> <ul> <li>`Table2_Syracuse2010_updated.pdf` and `Table2_Syracuse2010_updated.xlsx`: updated parameter values for the Syracuse et al., PEPI, 2010 global suite.</li> <li>`Table3_part_Syracuse2010_updated.pdf` and `Table3_part_Syracuse2010_updated.xlsx`: updated parameter values for the Syracuse et al., PEPI, 2010 global suite.</li> <li>`Figure_comp_D80_WW09_all.pdf`: a comparison between the Sepran models presented in `D80` and `D80new` and those in Wada & Wang, G-cubed, 2009.</li> <li>`Figure_comp_D80new_TF-Sepran_all.pdf`: comparison between the TerraFERMA and Sepran models presented in `D80new`.</li> <li>`Figure_III_6_all_D80.pdf`: complete set of model results for Figure 6, Part III.</li> <li>`Subduction_parameters.pdf` and `Subduction_parameters.json`: a description of the parameters used in the global suite.</li> <li>`PEPS_part_II_preprint.pdf`: preprint of part II.</li> <li>`PEPS_part_III_preprint.pdf`: preprint of part III.</li> <li>`vankeken_wilson_peps_2023_TF_lowres_minimal.zip`: contains a set of low resolution vtu files from TerraFERMA with the final potential temperature output from steady state and time dependent simulations. Intended for fast downloading (compared to `vankeken_wilson_peps_2023.zip`) and comparison.</li> </ul> <p><strong>Running a simulation</strong></p> <p>Input files are provided for the TerraFERMA (the Transparent Finite Element Rapid Model Assembler) simulations in this repository (`TF` subdirectories). Running them requires a working installation of TerraFERMA. If one is not available then consider using the docker image provided for this paper at:</p> <p>https://github.com/users/cianwilson/packages/container/package/vankeken_wilson_peps_2023</p> <p>This docker image contains a complete installation of TerraFERMA and its dependencies, PETSc, FEniCS and SPuD, within an Ubuntu 20.04LTS OS. For a full description of TerraFERMA please refer to the webpage:</p> <p>http://terraferma.github.io</p> <p> </p>
Kimberlite eruption driven by slab flux and subduction angle
<p>A supplementary data archive containing plate reconstruction files for use in GPlates. This plate model was modified from a recently-published model (1) as follows. Subduction zones to which no motions were assigned were initially stationary through time; these were assigned new motions relative to the global plate circuit to model moderate trench retreat while still remaining consistent with tomographic constraints. The Orcas plate was split into two separate plates at 170–130 Ma, consistent with its configuration after 130 Ma, in order to accommodate divergence at the plate boundaries. The Caribbean plate was also split by a new back-arc spreading centre at 140–120 Ma, to allow for the formation of the Caribbean large igneous province at a spreading ridge (2). Finally, the absolute plate motion model was constrained using an iterative optimisation workflow (3)</p> <p><strong>References</strong></p> <ol> <li>EJ Clennett, et al., A Quantitative Tomotectonic Plate Reconstruction of Western North America and the Eastern Pacific Basin. Geochem. Geophys. Geosystems 21, 1–25 (2020).</li> <li>A García-Reyes, J Dyment, Structure, age, and origin of the Caribbean Plate unraveled. Earth Planet. Sci. Lett. 571,<br> 117100 (2021).</li> <li>MG Tetley, SE Williams, M Gurnis, N Flament, RD Müller, Constraining Absolute Plate Motions Since the Triassic. J.<br> Geophys. Res. Solid Earth 124, 7231–7258 (2019).</li> </ol>
Model data repository of "Styles of Trench-parallel Mid-ocean Ridge Subduction Affect Cenozoic Geological Evolution in circum-Pacific Continental Margins"
<p>This dataset contains the data used in Wu et al. (2022): "Styles of Trench-parallel Mid-ocean Ridge Subduction Affect Cenozoic Geological Evolution in circum-Pacific Continental Margins".</p>
Aseismic and recent ruptures of persistent asperities along the Alaska-Aleutian subduction zone
<p>This repository contains GPS derived coseismic offsets and 87-day postseismic displacements associated with the 2020 Mw .78 Simeonof Island, Alaska earthquake, as well as the preferred interseismic backward slip rate distribution along the Alaska-Aleutian subduction zone in GMT psxy format. if you use the dataset, please cite the following paper:</p> <p>Zhao, B., Burgmann, R., Wang, D., Zhang, J., Yu, J., & Li, Q. (2022). Aseismic slip and recent ruptures of persistent asperities along the Alaska-Aleutian subduction zone. <em>Nature Communications</em>. https://doi.org/10.1038/s41467-022-30883-7</p>
ScienceDex guides
Understand access before you commit
These curated guides explain access requirements, typical timelines, costs, and reuse considerations for widely used research datasets.
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.
Annotated Behaviour and Observability Dataset (ABODe)
ABODe is a University of Edinburgh DataShare dataset for behavior classification in group-housed mice using home-cage video, identities, bounding boxes, ground-plate positions, and annotator labels.
DANDI Archive for NWB datasets
DANDI is a BRAIN Initiative archive for publishing and sharing neurophysiology data, including electrophysiology, optophysiology, and behavioral data packaged as NWB and related standards.
International Brain Laboratory public data
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.
OpenNeuro
OpenNeuro is a free, open platform for sharing neuroimaging datasets, with public search, dataset pages, and download paths for web, S3, DataLad, and the OpenNeuro CLI.