elongationvyöhyke
Elongationvyöhyke refers to a geological concept related to the deformation of rock layers, particularly in sedimentary basins. It describes the region where horizontal stretching and thinning of the crust occur, often leading to the formation of faults and grabens. This process is a key component in understanding basin evolution and the development of structural traps for hydrocarbons.
The elongation itself is a result of tensile forces acting on the Earth's crust. These forces can
In sedimentary basins, elongationvyöhyke is characterized by a series of parallel or en echelon normal faults.
Understanding the elongationvyöhyke is crucial for petroleum exploration. The structural traps formed by the faulting and