Mapeamento geológico da região de Reriutaba-CE

Abstract

The TransbrasilianLineament was an important geological phenomenon that left marks that can be seen to this day in america the continents of Africa and south. Due to its importance should be better studied and analyzed as it may be of great economic value geological goods to be found in these fractures. Off for example can be found once the fracture is old enough to generate this important element about everything these days where it can be a strategic asset that is for justification of war and conflict. The area studies this yours feature investigating in their litho-structural aspects of a region where we found lithologies and geological features with remnants of this action in lithologies. The region is located near the Transbrasilian lineament, suffering significant influence of the same, and you can see a large active structural activity in the area, expressed by fractures that are present both in the crystalline basement and in the sedimentary portions of the Great Sierra Group and Training Pacujá. The Precambrian crystalline basement occupies the southeast portion of the study area, often introducing himself with joints filled with granite and fractures in the granite itself with epidote bearing mafic among the lowest proportion of components.