Causes of slow earthquakes and multiple earthquakes.
نویسندگان
چکیده
منابع مشابه
Strain waves, earthquakes, slow earthquakes, and afterslip in the framework of the Frenkel-Kontorova model.
The one-dimensional Frenkel-Kontorova (FK) model, well known from the theory of dislocations in crystal materials, is applied to the simulation of the process of nonelastic stress propagation along transform faults. Dynamic parameters of plate boundary earthquakes as well as slow earthquakes and afterslip are quantitatively described, including propagation velocity along the strike, plate bound...
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ژورنال
عنوان ژورنال: Journal of Physics of the Earth
سال: 1980
ISSN: 1884-2305,0022-3743
DOI: 10.4294/jpe1952.28.169