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4 results for “Thermomechanical models”
Extracted experimental data for research paper titled "Micro-thermomechanical Modeling of Rocks with Temperature-dependent Friction and Damage Laws"
<p>This repository contains the experimental data on stress-strain curves extracted from the following original publications for constitutive model validation in our manuscript.</p> <p>[1] Jinping marble: Zhong, Y. Y. (2017). Research on mechanical properties of marble and the effects on rock burst under thermal-mechanical coupling (in Chinese) (Master’s thesis, Chengdu University of Technology). doi: 10.26986/d.cnki.gcdlc.2017.000109.</p> <p>[2] Beibei sandstone: Long, L. J. (2021). Study on mechanical and seepage properties of sandstone under the coupling of temperature-seepage-stress (in Chinese) (Doctoral dissertation, Chongqing University). doi: 10.27670/d.cnki.gcqdu.2021.001009.</p> <p>[3] Gongjue granite: Zhou, H. Y., Liu, Z. B., Shen, W. Q., Feng, T., & Zhang, G. Z. (2022). Mechanical property and thermal degradation mechanism of granite in thermal-mechanical coupled triaxial compression. International Journal of Rock Mechanics and Mining Sciences, 160, 105270. doi: 10.1016/j.ijrmms.2022.105270.</p>
Topography Response to Horizontal Slab Tearing and Oblique Continental Collision: 3D Thermomechanical Numerical Modelling
<p>This repository submission provides the 3D thermo-mechanical numerical modelling code I3ELVIS developed by the workgroup of Prof. Taras Gerya (ETH Zürich). The code is based on finite-difference and marker-in-cell methods (Gerya & Yuen, 2003, 2007; Gerya, 2019). The code solves the momentum, continuity, and energy equations on the fixed Eulerian grid and transports the physical properties by Lagrangian markers using the velocity field. The code also accounts for the major phase transitions in the Earth’s mantle and internal heat sources arising from adiabatic, radiogenic, and frictional heating. Partial melting and melt extraction processes are neglected for the sake of simplicity. A more detailed description of the code, including the governing equations and the adopted rheological model can be found in various published literature (Andrić-Tomašević et al., 2023; Boonma et al., 2023; Maiti et al., 2024). Interested users are recommended to contact Prof. Taras Gerya (taras.gerya@erdw.ethz.ch). </p> <p>The repository also provides input and output files to run and reproduce model results and manuscript figures of Maiti et al., 2024 (JGR Solid Earth). Paraview States for processing .vtr result files and visualizing the model output data. Matlab script to visualise the topography from .grd files. </p>
A 3-D kinematic ThermoMechanical model of the Central Andes Subduction Zone at 18°-26°S.
<p>These files contain physical parameters obtained with the preferred thermomechanical model presented in the paper:</p> <p><strong>J. Araya Vargas, J. Sanhueza & G. Yáñez (2021). The role of temperature in the along-margin distribution of volcanism and seismicity in subduction zones: insights from 3-D thermomechanical modelling of the Central Andean margin. Tectonics, 40(11), e2021TC006879. 10.1029/2021TC006879</strong></p> <p>The README file contains a description of the files, coordinate reference system, and a summary of the modeling setup. The detailed description of the employed thermomechanical modeling methodology is provided in the main text and Supporting Information of Araya Vargas, Sanhueza & Yáñez (2021).</p> <p>FILES:</p> <p>SZAndes18s26sTMmodel_temp.csv: whole model temperature<br> SZAndes18s26sTMmodel_dP.csv: mantle flow dynamic pressure.<br> SZAndes18s26sTMmodel_vx.csv: mantle flow velocity, X-axis component.<br> SZAndes18s26sTMmodel_vy.csv: mantle flow velocity, Y-axis component.<br> SZAndes18s26sTMmodel_vz.csv: mantle flow velocity, Z-axis component.</p> <p>DATABASES FIELDS:<br> pMPa = mantle flow dynamic pressure [MPa].<br> tempC = whole model temperature [°C].<br> VXmmyr = mantle flow velocity, X-axis component [mm/yr].<br> VYmmyr = mantle flow velocity, Y-axis component [mm/yr].<br> VZmmyr = mantle flow velocity, Z-axis component [mm/yr].<br> Xkm = X-axis position [km]. World Mercator coordinate system [EPSG code: 54004].<br> Ykm = Y-axis position [km]. World Mercator coordinate system [EPSG code: 54004].<br> Zkm = Z-axis position [km]. Z-coordinate is reported as height from the mean sea level.</p>
Dataset for Effects of elasticity on subduction initiation: Insight from 2-D thermomechanical models
<p>Numerical modeling results and input files of the manuscript "Effects of elasticity on subduction initiation: Insight from 2-D thermomechanical models".</p>
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OpenNeuro
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