WadatiBenioffzónában
A WadatiBenioffzóna, often referred to as a Benioff Zone, is a planar zone of shallow, intermediate, and deep earthquake activity that occurs in relation to a convergent plate boundary. This phenomenon is a direct consequence of subduction, where one tectonic plate slides beneath another and sinks into the Earth's mantle. As the subducting plate descends, it generates friction and stress, leading to the release of seismic energy in the form of earthquakes.
The WadatiBenioff Zone is characterized by a dipping arrangement of these earthquakes. The shallowest earthquakes occur
The identification and mapping of WadatiBenioff Zones are crucial for understanding plate tectonics and seismic hazard