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false4DOIDB.GFZ 10.5880/GFZ.1.3.2020.001 Petrunin, Alexey Alexey Petrunin 0000-0002-5439-4178 GFZ German Research Centre for Geosciences, Potsdam, Germany Kaban, Mikhail Mikhail Kaban 0000-0002-1864-2234 GFZ German Research Centre for Geosciences, Potsdam, Germany The mantle flow velocity and maximum principal stress orientation calculated by use of a geodynamical model GFZ Data Services 2020 Geodynamic model calculated velocity field maximum principal stress EARTH SCIENCE > SOLID EARTH > TECTONICS > PLATE TECTONICS > STRESS EARTH SCIENCE > SOLID EARTH > TECTONICS EARTH SCIENCE > SOLID EARTH Petrunin, Alexey Alexey Petrunin 0000-0002-5439-4178 GFZ German Research Centre for Geosciences, Potsdam, Germany Kaban, Mikhail Mikhail Kaban 0000-0002-1864-2234 GFZ German Research Centre for Geosciences, Potsdam, Germany en 10.1029/2019TC005829 1 Files application/octet-stream CC BY 4.0 In the data set we provide both mantle velocity and maximum principal stress orientation resulting from a geodynamical model. The data are calculated with use of the ProSpher 3D code in a spectral domain by spherical harmonics decomposition. The resolution of the model is of 120 spherical harmonics laterally and 50 km in depth. For velocity data (file set: Petrunin-etal19-Vel_XXX.dat), the 1st column represents longitude, 2nd column – latitude, 3d, 4th , 5th – longitudinal, latitudinal, and radial components of velocity in mm/yr, correspondingly. For maximum principal stress orientation data (file set: Petrunin-etal19-SH_XXX.dat), the 1st column represents longitude, 2nd column – latitude, 3d, 4th – longitudinal and latitudinal components of the unit vector representing maximum principal stress direction. 24 67 2 47 Deutsche Forschungsgemeinschaft http://doi.org/10.13039/501100001659 SPP 2017 Mountain Building Process in Four Dimensions (4D-MB)