Subduction thermal modeling in Makran

Published: 8 February 2024| Version 1 | DOI: 10.17632/cgdww9bvbf.1
Contributor:
Yingfeng Ji

Description

The data includes the three-dimensional temperature field (degrees Celsius), water content (wt%), dehydration rate (wt%/km), rock phase change distribution, and subduction velocity field (cm/yr) of the subducting plate, as well as the coastline and volcano distribution. The data source method is a three-dimensional finite-difference numerical simulation. The geophysical calculation is ensured after the subduction thermal regime reaches a steady state. The temperature field error range is ±10 degrees Celsius, and the velocity field error range is ±0.1cm/ yr. This data can be further used analyzing the geophysical field of subduction zone. File naming: the data is stored in text paraview format. Data reading method: All ASCII code files in the data set can be directly opened with paraview software. Data list: 1. eq_USGS.vtk (Earthquake Catalog by IRIS, 2000-2010, Trabant et al., 2012) http://ds.iris.edu/ieb/ 2. state.vtk (country boudaries, GMT, Wessel and Smith, 1998) 3. volcano.vtk (global volcanoes at NCEI, Siebert et al., 2010) 4. plate_boundary.vtk (global plate boundaries, Bird, 2003) 5. box.vtk (model region, this study) 6. slab.vtk (3-D thermal regime, slab water content and slab dehydration, this study)

Files

Institutions

Institute of Tibetan Plateau Research Chinese Academy of Sciences

Categories

Geodynamics

Licence