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215 results for “Slab”
Dataset for: "Effect of the Cold Nazca Slab on the Depth of the 660km Discontinuity in South America"
<p>This dataset contains the resulting <strong>stacked receiver functions</strong>,<strong> interpreted times</strong> (as tables and grids), and <strong>derived depths</strong> (as tables and grids) for the <strong>410 km and 660 km discontinuities </strong>across the whole <strong>South America Continent</strong>. It also contains considered piercing point positions used for stacking and also a derived grid for the transition zone thickness along with seismic sections PDF files. This dataset is detailed described and discussed by the article entitled “<em>Effect of the Cold Nazca Slab on the Depth of the 660 km Discontinuity in South America</em>" published by the Journal of South American Earth Sciences in the year 2021 under DOI <a href="https://dx.doi.org/10.1016/j.jsames.2021.103607">10.1016/j.jsames.2021.103607</a>.</p> <p>For a complete description of the available data check the included `README` file. Binary files use standard formats that can be open using standard open software. Files checksum are available in the MD5SUM file.</p>
Pervasive hydrous carbonatitic liquids mediate transfer of carbon from the slab to the subarc mantle
<p>Table S1:Compositions of starting materials and global subducting sediments; Table S2: Experimental run conditions and phase assemblage; Table S3-12:Electron microprobe analyses of experimental products</p>
Pervasive hydrous carbonatitic liquids mediate transfer of carbon from the slab to the subarc mantle
<p>File Name: Supplementary table 1</p> <p>Description: Compositions of starting materials and global subducting sediments</p> <p>File Name: Supplementary table 2</p> <p>Description: Experimental run conditions and phase assemblage</p> <p>File Name: Supplementary Data 1<br> Description: Electron microprobe analyses of silicate melt and carbonated silicate melt</p> <p>File Name: Supplementary Data 2<br> Description: Electron microprobe analyses of quenched carbonate</p> <p>File Name: Supplementary Data 3<br> Description: Electron microprobe analyses of equilibrium carbonates</p> <p>File Name: Supplementary Data 4<br> Description: Electron microprobe analyses of glass spheres</p> <p>File Name: Supplementary Data 5<br> Description: Electron microprobe analyses of bulk compositions of quenched liquids</p> <p>File Name: Supplementary Data 6<br> Description: Electron microprobe analyses of garnet</p> <p>File Name: Supplementary Data 7<br> Description: Electron microprobe analyses of clinopyroxene</p> <p>File Name: Supplementary Data 8<br> Description: Electron microprobe analyses of phengite</p> <p>File Name: Supplementary Data 9<br> Description: Electron microprobe analyses of kyanite</p> <p><br> File Name: Supplementary Data 10<br> Description: Electron microprobe analyses of magnetite</p>
Pervasive hydrous carbonatitic liquids mediate transfer of carbon from the slab to the subarc mantle
<p>File Name: Supplementary Data 1<br> Description: Electron microprobe analyses of silicate melt and carbonated silicate melt</p> <p>File Name: Supplementary Data 2<br> Description: Electron microprobe analyses of quenched carbonate</p> <p>File Name: Supplementary Data 3<br> Description: Electron microprobe analyses of equilibrium carbonates</p> <p>File Name: Supplementary Data 4<br> Description: Electron microprobe analyses of glass spheres</p> <p>File Name: Supplementary Data 5<br> Description: Electron microprobe analyses of bulk compositions of quenched liquids</p> <p>File Name: Supplementary Data 6<br> Description: Electron microprobe analyses of garnet</p> <p>File Name: Supplementary Data 7<br> Description: Electron microprobe analyses of clinopyroxene</p> <p>File Name: Supplementary Data 8<br> Description: Electron microprobe analyses of phengite</p> <p>File Name: Supplementary Data 9<br> Description: Electron microprobe analyses of kyanite</p> <p><br> File Name: Supplementary Data 10<br> Description: Electron microprobe analyses of magnetite</p>
Data for "Ultra-low-velocity anomaly inside the Pacific Slab near the 410-km discontinuity"
<p>This folder contains the P- and S-wave displacement records after removing the instrument responses.</p> <p>./20091010_RR_Pwave : P-wave data for the reference region of event 20091010.<br> ./20091010_SS1_Pwave : P-wave data for the SS1 region of event 20091010.<br> ./20091010_SS2_Pwave : P-wave data for the SS2 region of event 20091010.<br> ./20090407_Pwave : P-wave data of event 20090407.<br> ./20110804_Pwave : P-wave data of event 20110804.<br> ./20091010_Swave : S-wave data of event 20091010.</p>
Geometrical Relations between Slab Dip and the Location of Volcanic Arcs and Back-arc Spreading Centers
<p>The dataset includes the measurements of individual subduction zones defined in the convergence-parallel, trench-perpendicular, and spreading-parallel direction. </p> <p> </p> <p>Table S3. Location of each trench, arc, and back-arc defined in a direction parallel to the convergence, and the corresponding distance from the trench to the arc (D_TA), subarc slab depth (H), and from the trench to the back-arc spreading center (D_TB). The slab dip is measured at 50km (Dip50), 100km (Dip100), and 200km (Dip200) and averaged from 0 to 50 km (Dip050), 0 to 100km (Dip0100), 0 to 200km (Dip0200), and 50 to 200km (Dip50200). </p> <p>Table S4. Location of each trench, arc, and back-arc defined in a direction perpendicular to the trench, and the corresponding distance from the trench to the arc (D_TA), subarc slab depth (H), and from the trench to the back-arc spreading center (D_TB). The slab dip is measured at 50km (Dip50), 100km (Dip100), and 200km (Dip200) and averaged from 0 to 50 km (Dip050), 0 to 100km (Dip0100), 0 to 200km (Dip0200), and 50 to 200km (Dip50200). </p> <p>Table S5. Location of each trench, arc, and back-arc defined in a direction parallel to the spreading direction, and the corresponding distance from the trench to the arc (D_TA), subarc slab depth (H), and from the trench to the back-arc spreading center (D_TB). The slab dip is measured at 50km (Dip50), 100km (Dip100), and 200km (Dip200) and averaged from 0 to 50 km (Dip050), 0 to 100km (Dip0100), 0 to 200km (Dip0200), and 50 to 200km (Dip50200). </p> <p> </p>
Deep subduction of the Philippine Sea slab and formation of slab window beneath central Japan
<p>The travel-time data, the velocity model from seismic tomography and the temperature distributions from numerical simulation.</p>
Parameter files for 3-D plume-slab interaction models
<p>Parameter files used in ASPECT for the four models presented in "Plume-driven subduction termination in 3-D mantle convection models"</p>
Transient Injection of Flow: How Torn and Bent Subducting Slabs Induce Unusual Mantle Circulation Patterns near a flat slab
<p>This repository provides the input (.prm) files for the paper "Transient Injection of Flow: How Torn and Bent Slabs Induce Unusual Mantle Circulation Patterns near a flat slab".</p>
Supplementary for Slab tearing and lithospheric structures in Luzon island, Philippines: Constraints from P-and S-wave local earthquake tomography
<p>The 3D seismic velocity model of the Northern Philippines was obtained from travel time inversion using LOTOS (Koulakov., 2009). </p> <p>The header of the file is:</p> <p>lon: longitude</p> <p>lat: latitude</p> <p>dep: depth in km</p> <p>vp_abs: absolute P-wave velocity (km/s)</p> <p>vs_abs: absolute S-wave velocity (km/s)</p> <p>dvp: P-wave velocity anomalies (%)</p> <p>dvs: S-wave velocity anomalies (%)</p> <p> </p>
Data of "Towards linking slab window geodynamics with the geophysical and geochemical signature of the upper mantle", Sanhueza et al. EPSL
<p><strong>Description for sanhuezaetal_epsl_ternary.zip</strong><br> These files contain a high resolution figure and a script to reproduce the ternary diagram (Figure 5d) of the paper:</p> <p>Sanhueza et al. Towards linking slab window geodynamics with the geophysical and geochemical signature of the upper mantle, <br> under review in Earth and Planetary Science Letters.</p> <p>A high resolution figure of the ternary diagram is provided (sanhuezaetal_EPSL_ternary.pdf).</p> <p>In addition, the MATLAB script to plot this diagram is included.<br> This script (ternary_plot.m) uses 4 files: temp_RGB.txt, melt_RGB.txt, matrix_RGB.txt, rminmax_RGB.txt</p> <p><br> FILE LIST<br> sanhuezaetal_EPSL_ternary.zip<br> -sanhuezaetal_EPSL_ternary.pdf - High resolution Figure 5d of the manuscript<br> -ternary_plot.m - MATLAB script to generate Figure 5d<br> -temp_RGB.txt - Normalized temperatures in the r-alpha space<br> -melt_RGB.txt - Normalized upward melt flux in the r-alpha space<br> -matrix_RGB.txt - Normalized upward matrix flux in the r-alpha space<br> -rminmax.txt - Envelope of r = rcmin and r = rcmax<br> </p> <p>---------------------------------------------------------------------------------------------------------------------------------------------------------------</p> <p><strong>Description for sanhuezaetal_epsl_3dmodelresults.zip</strong><br> These files contain 3D model results presented in the manuscript:</p> <p>Sanhueza et al. Towards linking slab window geodynamics with the geophysical and geochemical signature of the upper mantle, <br> under review in Earth and Planetary Science Letters.</p> <p>These files were obtained after interpolating the model in a regular grid with cells of 10 km x 10 km x 10 km.</p> <p><br> FILE LIST<br> sanhuezaetal_EPSL_results.zip</p> <p>a0r1_Tvxvyvz.txt, a0r2_Tvxvyvz.txt a0r05_Tvxvyvz.txt<br> a10r1_Tvxvyvz.txt, a10r3_Tvxvyvz.txt, a10r04_Tvxvyvz.txt<br> a20r1_Tvxvyvz.txt, a20r2_Tvxvyvz.txt, a20r05_Tvxvyvz.txt<br> a30r1_Tvxvyvz.txt, a30r07_Tvxvyvz.txt, a30r15_Tvxvyvz.txt<br> a45r1_Tvxvyvz.txt, a45r08_Tvxvyvz.txt, a45r12_Tvxvyvz.txt<br> a60r1_Tvxvyvz.txt, a70r1_Tvxvyvz.txt</p>
SMAP-derived Perennial Firn Aquifer and Ice Slab Extents 2015-2019 Version 1
<p>SMAP-derived Perennial Firn Aquifer and Ice Slab Extents 2015-2019 Version 1</p>
Subduction thermal regime, slab dehydration, and seismicity distribution beneath Hikurangi based on 3-D simulations
Open the record for dataset details and reuse information.
Thermal state, slab metamorphism and interface seismicity in the Cascadia subduction zone based on 3-D modeling
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Slab metamorphism and interface earthquakes in Peru: implications for along-strike fluid content and seismotectonic variation
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Slab Ocean forcing file and model output for "Seasonal Transitions and the Westerly Jet in the Holocene East Asian Summer Monsoon"
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SLABCC: Total energy correction code for charged periodic slab models
<p>Test set for SLABCC (SLAB Charge Correction) including the input files, input parameters and the expected output.<br> The geometries correspond to the positively charged Cl-vacancy on the surface of the NaCl slab with different vacuum thickness. The compiler type/compilation flags, linked libraries, and the hardware architecture may influence the optimization results but the effects on the correction energies should be negligible.</p> <p>The latest version of SLABCC can be downloaded from <a href="https://github.com/MFTabriz/slabcc">https://github.com/MFTabriz/slabcc</a></p> <p> </p>
Transient stripping of subducting slabs controls periodic forearc uplift
<p>This Source-Data file contains output files from numerical experiments presented by Menant et al. in a study published in Nature Communications (i.e., Transient stripping of subducting slabs controls periodic forearc uplift; doi: 10.1038/s41467-020-15580-7). MATLAB codes to post-process these files are also provided.</p> <p>The source code is available from the corresponding author (armel.menant@gfz-potsdam.de) or from the main code developer (taras.gerya@erdw.ethz.ch) upon reasonable request.</p>
Slab dehydration in Sumatra: Implications for fast and slow earthquakes and arc magmatism
<p>The catastrophic 2004 Sumatra-Andaman Mw9.1 earthquake associated with destructive tsunamis has characterized Sumatra as one of the most dangerous convergence zones. Nevertheless, the effects of the thermohydrous state on the strongly coupled megathrust of the incoming plate remain enigmatic. By using a 3-D thermomechanical model to compute the temperature variation and the complicated phase transition process of the water-bearing descending plate which generates unstable thrust slips, we find that Sumatran earthquakes at varying depths are likely under the control of the inter- or intraplate hydrothermal regime, which occurs in or close to the petrological metamorphism transition area. The slab dehydration of the water-rich mid-ocean-ridge basalts (MORB) and the ultramafic rocks in the oceanic lithosphere releases a large amount of fluid to the continental wedge and further facilitates arc magmatism. The fluids are prone to upwelling following the subduction channel along the plate interface and thus contribute to the clustering of earthquakes updip of the dehydration front beneath offshore Sumatra. Brittle failure and dehydration embrittlement at depth, along with the temperature differences caused by variant slab geometry, are conjectured to greatly influence the occurrence of fast and slow earthquakes in Sumatra.</p>
Data for the article: Residual Flexural Performance of Large-Scale Ferronickel Slag Alkali-Activated Concrete Slabs After Fire Exposure
<p>Figures and related data for the article Residual Flexural Performance of Large-Scale Ferronickel Slag Alkali-Activated Concrete Slabs After Fire Exposure</p>
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