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1.2.-How-Do-Earthquakes-Happen__-CE-305
Comparison of geodetic slip-deficit and geologic fault slip rates reveals that variability of elastic strain accumulation and release rates on strike-slip faults is controlled by the relative structural complexity of plate-boundary fault
PHYSICAL MECHANISM OF MAJOR EARTHQUAKES BY EARTHQUAKE CASES ANALYSIS
1 -Modèle du rebond élastique pensé par Reid (1910) pour expliquer
Schematic illustration of elastic rebound hypothesis (Reid, 1910; Jiang
PDF) PHYSICAL MECHANISM OF MAJOR EARTHQUAKES BY EARTHQUAKE CASES
The concept of elastic-rebound theory with a sketch and an example to illustrate the concept (other than a rubber band).
wu XIAOWA, Doctor, PhD
Elastic Rebound and Earthquake Source Models: Vertical Strike-Slip Faults, Slides Geology
GeoHazards, Free Full-Text
Present-day kinematic behaviour of active faults in the Eastern Alps - ScienceDirect