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The gravity and magnetic anomalies, as well as the inferred source bodies that produce those geophysical anomalies, lie between the Sontecomapan and Catemaco faults, which are proposed as flower structures associated with an inferred deep-seated fault termed the Veracruz Fault.
Accordingly and taking into consideration the facial association changes, biostratigraphic zonation and lithostratigraphic markers, the effects of the Sirwan (Khanaqin) fault and Greater Zab deep-seated fault were proposed as controlling factors of the palaeo-configurations and palaeo-geographic distribution of the trough and platform settings.
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At that time, ice-stream routing in the Disko Bay shelf region was strongly controlled by the pre-glacial topography and structural boundaries associated with fracture zones and deep-seated faults.
New Madrid Seismic Zone (NMSZ), region of poorly understood, deep-seated faults in Earth's crust that zigzag southwest-northeast through Arkansas, Missouri, Tennessee, and Kentucky, U.S. Lying in the central area of the North American Plate, the seismic zone is about 45 miles (70 km) wide and about 125 miles (200 km) long.
The blocks lying between the deep-seated faults are also deformed by the right-lateral transpression.
The distance between each of the northern five deep-seated faults is approximately 15 km.
Benin and Calabar Hinge lines are the deep-seated faults associated with the rifting controlled formation of the delta.
Therefore, Gebel El Maghara belongs to the deformed block lying between the second and third deep-seated faults.
The axes of these three major structures and their accompanying thrusts make acute angles with the deep-seated faults.
The right stepping of the folds indicates that the strike-slip movement on the deep-seated faults was right lateral.
This shear couple has probably caused the right-lateral rejuvenation of the deep-seated faults in the northern Egypt.
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