Subduction thermal modeling in Makran

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)