2026-04-06T09:07:07Zhttp://doidb.wdc-terra.org/oaip/oai

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false4DOIDB.WSM 10.5880/wsm.2021.003 Ziegler, Moritz O. Moritz O. Ziegler 0000-0002-2288-2820 GFZ German Research Centre for Geosciences, Potsdam, Germany Heidbach, Oliver Oliver Heidbach 0000-0001-8009-5422 GFZ German Research Centre for Geosciences, Potsdam, Germany GFZ Data Services 2021 geomechanical-numerical model stress in-situ stress model calibration stress tensor calibration modelling tool EARTH SCIENCE > SOLID EARTH > TECTONICS > NEOTECTONICS EARTH SCIENCE > SOLID EARTH > TECTONICS > PLATE TECTONICS > CRUSTAL MOTION > CRUSTAL MOTION DIRECTION EARTH SCIENCE > SOLID EARTH > TECTONICS > PLATE TECTONICS > FAULT MOVEMENT EARTH SCIENCE > SOLID EARTH > TECTONICS > PLATE TECTONICS > PLATE BOUNDARIES EARTH SCIENCE > SOLID EARTH > TECTONICS > PLATE TECTONICS > STRESS Ziegler, Moritz O. Moritz O. Ziegler 0000-0002-2288-2820 GFZ German Research Centre for Geosciences, Potsdam, Germany Ziegler, Moritz O. GFZ German Research Centre for Geosciences, Potsdam, Germany Ziegler, Moritz O. GFZ German Research Centre for Geosciences, Potsdam, Germany Software 10.48440/wsm.2021.003 10.5880/wsm.2021.002 10.5880/wsm.2016.001 10.1186/s40517-020-00178-5 10.5880/wsm.2020.001 https://www.tecplot.com/products/tecplot-360/ 10.5194/se-7-1365-2016 https://github.com/MorZieg/PyFAST_Calibration https://mooseframework.inl.gov/ 1.0 GNU General Public License Version 3 (29 June 2007); Copyright (C) 2021 Helmholtz Centre Potsdam GFZ German Research Centre for Geosciences, Potsdam, Germany The 3D geomechanical-numerical modelling of the in-situ stress state aims at a continuous description of the stress state in a subsurface volume. It requires observed stress information within the model volume that are used as a reference. Once the modelled stress state is in agreement with the observed reference stress data the model is assumed to provide the continuous stress state in its entire volume. The modelled stress state is fitted to the reference stress data records by adaptation of the displacement boundary conditions. This process is herein referred to as calibration. Depending on the amount of available stress data records and the complexity of the model the manual calibration is a lengthy process of trial-and-error modelling and analysis until best-fit boundary conditions are found.

The Fast Automatic Stress Tensor Calibration (FAST Calibration) is a Python function that facilitates and speeds up this calibration process. By using a linear regression it requires only three model scenarios with different boundary conditions. The stress states from the three model scenarios at the locations of the reference stress data records are extracted. The differences between the modelled and observed stress states are used for a linear regression that allows to compute the displacement boundary conditions required for the best-fit modelled stress state. If more than one reference stress state is provided, the influence of the individual observed stress data records on the best-fit boundary conditions can be weighted.

GNU General Public License, Version 3, 29 June 2007

Copyright © 2021 Helmholtz Centre Potsdam GFZ German Research Centre for Geosciences, Potsdam, Germany

PyFAST Calibration is free software: you can redistribute it and/or modify it under the terms of the GNU General Public License as published by the Free Software Foundation, either version 3 of the License, or (at your option) any later version.

PyFAST Calibration is distributed in the hope that it will be useful, but WITHOUT ANY WARRANTY; without even the implied warranty of MERCHANTABILITY or FITNESS FOR A PARTICULAR PURPOSE. See the GNU General Public License for more details. You should have received a copy of the GNU General Public License along with this program. If not, see http://www.gnu.org/licenses/.

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