The researchers determined that the earthquakes at Abu Dabbab extend in a line from the coast into the Red Sea, «and the seismicity pattern is arc - shaped in depth, confined to the dome - like structure of
the rigid igneous body that formed during the Precambrian era» above an active fault, El Khrepy said.
The finding about continents jibes with evidence from
igneous rocks — those sourced in hot, molten rock — which indicated that the surface became
rigid enough to support mountain belts, which would have eroded, during this period.