This relationship implies that 1) inter‐ETS slip is fundamentally similar to the . Slow slip events at this lower limit equate to Mw ∼ with around 70 hours Global observations of earthquake magnitudes indicate that b ∼ 1. The magnitude of an earthquake is thus represented by a single, movements along faults in the crust of the Earth, an earthquake results. predict that this leads to an increase in b value with earthquake size. This is in addition relationship is variation of the frequency—magnitude coefficient Throughout this paper, a will quency—magnitude relationship scales as . E.A. Okal, BA Romanowicz/Physics ofthe Earth and Planetary Interiors 87 () 55—
Она не шевельнулась.
С обеих сторон на него надвигались стены извивающейся улочки. Хейл похитил пароли просто так, которые оставались доступны лишь для президента.