Extensional Tectonic Regime Free 3D model
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Researchers have identified that principal stress axes are oriented in specific directions within extensional tectonic environments, characterized by a decrease in the overall rock volume. This orientation is determined by various factors, including the magnitude and direction of tensile forces, the type of rocks present, and their initial state of stress. By analyzing these variables, scientists can reconstruct the evolution of deformation within these areas, ultimately providing insights into the processes that govern mountain building.
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