The strong tectonic forces that occur within the earth are typically what cause geologic structures. These forces result in deep faults, rock folding and breaking, and mountain formation.
The study of the three-dimensional distribution of rock units in relation to their deformational histories is known as structural geology. The main objective of structural geology is to understand the stress field that produced the observed strain and geometries by using measurements of the current rock geometries to learn about the history of deformation (strain) in the rocks.
A common objective is to comprehend the structural evolution of a specific region with respect to regionally widespread patterns of rock deformation (for example, mountain building, rifting) caused by plate tectonics. This understanding of the dynamics of the stress field can be linked to significant events in the geologic past.
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