The geological structure of the geological sciences who learned about the form (architecture) as a result of rock deformation system. systems that change shape deformation as well as the size of the rocks result of force (force) which took place in the earth. the force is in principle a tectonic system that goes inside the earth. in a general sense, the geological composition of the science learned about rocks form as the crust side of the system and explain its formation.
most authors assume that the geological structure is preferred to the study of the geological composition of the elements, for example, multiplicity (fold), fracture (fracture), faults (fault), and so on, as the side of a tectonic unit (tectonic unit), but the tectonic and geotectonic mistaken for one study with an increasingly large scale, the geological study objects like sedimentation basin, the mountains, the ocean floor, and so on.
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