This paper discusses studies of the migration over time of hypocenters from great depths to the Earth’s surface. The calculations are based on the notion that surface fracturing of the external lithosphere corresponds to brittle fracturing, while internal lithosphere fracturing, accompanied by a decrease of earthquake hypocenter depth, corresponds to ductile fracturing. A procedure for calculating periods of the rising of earthquake sources in an elastic-plastic environment is suggested. Finally, it was revealed that the rising of hypocenters to the surface takes approximately 8–10 years.
Office TS-34, Department of Physics of the Earth, Faculty of Physics, Moscow State University, Moscow, 119991, Russia
Science News of the Faculty of Physics, Lomonosov Moscow State University
This new information publication, which is intended to convey to the staff, students and graduate students, faculty colleagues and partners of the main achievements of scientists and scientific information on the events in the life of university physicists.