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16 results for “continental subduction,”
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>
Code and Velocity Data for Sustained indentation in 2D models of continental collision involving whole mantle subduction
<p>Contains the Python code for all models and resolution tests using the <a href="https://www.underworldcode.org/intro-to-underworld">underworld geodynamics code</a> in "Sustained indentation in 2D models of continental collision involving whole mantle subduction" submitted to GJI</p>
Lithosphere tearing and foundering during continental subduction: insights from Oligocene-Miocene magmatism in southern Tibet
<p>Table S1. Major and trace elements and age data summary.</p> <p>Table S2. Zircon U-Pb ages.</p> <p>Table S3. Mineral major elements.</p> <p>Table S4. Zircon trace elements.</p> <p>Table S5. Published ages of the Oligocene to Miocene igneous rocks in southern Tibet</p> <p>Table S6. Calculated primary magmas and P estimates of the ultrapotassic rocks in southern Tibet.</p>
2D visco-elasto-plastic subduction models in the presence of a high density and viscosity continental block
<p>Three main models with different rheological conditions and density are incorporated for an imposed intrusion between the upper and lower continental crust. Output files for a model with a crust without intrusions are also incorporated.</p> <p>The file contains data on the conditions of plate motion velocity, plate age, plate thickness in Excel (Input_Data_Age_Vel.xlsx), a table with the rheology used to reproduce different numerical models incorporating the intrusion (Table_S3.pdf), and a file High_density_materials.m showing the construction of the intrusion within the continental crust.</p> <p>High_density_materials.m m should be imposed on the original I2ELVIS code provided by Taras Gerya - ETH Zürich, Institut für Geophysik, Switzerland - email: taras.gerya@erdw.ethz.ch</p> <p>The file has the main time steps as a function of temperature, viscosity, density and rock composition into the folders. If you want to visualize them please run the following Script PLOT_OUTPUT_DATA.m where,</p> <p>str=string(2040), represent the time_step</p> <p>Files are organized in a matrix form, each folder has the</p> <p>grid_x :coordinate matrix, <br>gridy_: coordinate matrix, </p> <p>matrix_temperature_, density and viscosity.</p> <p>To plot the Rock composition.</p> <p>mx and my, tracer coordinates in x-direction and y-direction<br>matrix_markcom is matrix tracers.</p> <p> </p> <p>Model 1</p> <p>(Time step= 10= 14.99 Ma, 120= 14 Ma, 310= 12 Ma, 670 = 9 Ma, 1120 = 6 Ma, 1620 = 3 Ma, 2040 = 0 Ma)</p> <p> </p> <p>The temperature, viscosity, density, and rock composition for the PHS slab are shown in this animation for Model 1. <br>This model is reproduced under the conditions of plate motion velocity and age from Figure 3 with an initial dip angle for the weak zone of 20°. <br>The high density material between the upper and lower crust in the vicinity of the slab is not included in Model 1. <br>The model evolves over a period of the last 15 Myr and shows a shallow subduction. </p> <p><br>Model 2</p> <p>(Time step= 10= 14.99 Ma, 120= 14 Ma, 380= 12 Ma, 850 = 9 Ma, 1490 = 6 Ma, 2090 = 3 Ma, 2540 = 0 Ma)</p> <p>With high density block<br>The temperature, viscosity, density, and rock composition for the PHS slab are shown in this animation for Model 2. This model is reproduced under the conditions of plate motion velocity and age from Figure 3 with an initial dip angle for the weak zone of 20°. The high density material between the upper and lower crust in the vicinity of the slab is included in Model 2. The model evolves over a period of the last 15 Myr and shows a steep subduction.</p> <p><br>Model 3</p> <p>(Time step= 10= 14.99 Ma, 120= 14 Ma, 310= 12 Ma, 670 = 9 Ma, 1120 = 6 Ma, 1690 = 3 Ma, 2040 = 0 Ma)</p> <p>Without high density block and high viscosity</p> <p>The temperature, viscosity, density, and rock composition for the PHS slab are shown in this animation for Model 3. This model is reproduced under the conditions of plate motion velocity and age from Figure 3 with an initial dip angle for the weak zone of 20°. The initial high viscosity material and without high density between the upper and lower crust in the vicinity of the slab is included in Model 3. The model evolves over a period of the last 15 Myr and shows subduction with a high dip angle. </p> <p><br>Model4</p> <p>(Time step= 10= 14.99 Ma, 120= 14 Ma, 330= 12 Ma, 770 = 9 Ma, 1190 = 6 Ma, 1640 = 3 Ma, 2040 = 0 Ma)<br> <br>With high density block and high viscosity<br>The temperature, viscosity, density, and rock composition for the PHS slab are shown in this animation for Model 4. This model is reproduced under the conditions of plate motion velocity and age from Figure 3 with an initial dip angle for the weak zone of 20°. The high density and high viscosity material between the upper and lower crust in the vicinity of the slab is included in Model 4. The model evolves over a period of the last 15 Myr and shows a steep subduction</p>
Deep Subduction Versus Collision Cessation: The Fate of Continental Collisional Orogens
<p>Deep Subduction Versus Collision Cessation: The Fate of Continental Collisional Orogens</p>
Dataset for Overriding lithospheric strength affects continental collisional mode selection and subduction transference: Implications for Greater
<p>This .zip file is the relative dataset for the models of <strong>Overriding lithospheric strength affects continental collisional mode selection and subduction transference: Implications for Greater India-Asia convergent system.</strong></p>
Tracing the oxidizing state and element-mobilizing fluids in continental subduction zones:Insights from the granitic melt-eclogite interface
Open the record for dataset details and reuse information.
Datasets: Wedge-shaped southern Indian continental margin without proper weakness hinders subduction initiation
<p>The numerical model results of "Wedge-like southern Indian continental margin without proper weakness hinders subduction initiation".</p>
Nature of Paleo-Pacific subduction along the East Asian continental margin Insights from the sedimentary record of West Sarawak,Borneo
<p>The Table S1, S2, S3, S4 in the manuscript "Nature of Paleo-Pacific subduction along the East Asian continental margin: Insights from the sedimentary record of West Sarawak, Borneo"</p>
Dataset for "continental tip is a favorable location for subduction initiation"
<p>The required code and data for the paper "continental tip is a favorable location for subduction initiation"<br> The open-source code Ellipsis3d is also available at https://geodynamics.org/resources/ellipsis3d<br> The reconstruction of Oloy subduction is also available at doi:10.1016/j.earscirev.2013.05.012<br> </p>
Supplementary material for "The signature of lithospheric anisotropy at post-subduction continental margins: new insight from XKS splitting analysis in northern Borneo"
<p><strong>Supplementary material for the manuscript "The signature of lithospheric anisotropy at post-subduction continental margins: new insight from XKS splitting analysis in northern Borneo" by Bacon, C.A., Rawlinson, N., Pilia, S., Gilligan, A., Wehner, D., Cornwell, D.G., and Tongkul, F., submitted for publication in Geochemistry, Geophysics, Geosystems.</strong><br> <br> The material has been divided into 3 directories:</p> <ul> <li><em>a_supplementary_datafiles </em>- datafiles listed in the supplementary file accompanying the manuscript</li> <li><em>b_2018-2020</em> - SplitRacer directory for the time period of the nBOSS network deployment, containing: <ul> <li>Cut and bandpass filtered waveforms</li> <li>Metadata files required to run SplitRacer</li> <li>Splitting results (single splitting and joint splitting, where possible)</li> </ul> </li> <li><em>c_2006-2020 </em>- SplitRacer directory for the time period of the KKM/LDM permanent station deployments, containing: <ul> <li>Cut and bandpass filtered waveforms</li> <li>Metadata files required to run SplitRacer</li> <li>Splitting results (single splitting and joint splitting, where possible)</li> </ul> </li> </ul> <p>Directories <em>b </em>and <em>c </em>are valid SplitRacer projects that can be loaded directly and processed from the measurement stage onward.</p>
Supplementary Data for Forced Cenozoic continental subduction of Tarim craton-like lithosphere below the Tianshan revealed by ambient noise tomography
<p>Please read the README.txt file for more information.</p>
Tracing the oxidizing state and element-mobilizing fluids in continental subduction zones:Insights from the granitic melt-eclogite interface
Open the record for dataset details and reuse information.
A new magmatic record of Indian continental subduction beneath the Lhasa terrane at ca. 50 Ma: evidence from the ultrapotassic–potassic dikes in the Lhasa terrane
<p>Tables S1-S8</p>
Subductability of continental lithosphere
<p>Dataset for subductability of continental lithosphere</p>
Dual subduction zones of the Neo-Tethys Ocean recorded by Late Cretaceous continental arc magmatism in southern Tibet
<p><span>Supporting Information </span> </p>
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International Brain Laboratory public data
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OpenNeuro
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