I. Energy Ratio of the Seismic Waves Reflected and Refracted at a Rock Water Boundary. II. Amplitudes of PcP, PcS, ScS, and ScP in Deep-Focus Earthquakes
<p>Part I.</p> <p>Using the Knott-Zoeppritz equations, the general behavior, zero points and extreme points of the energy ratio that goes into reflected and refracted waves upon the incidence of a wave at either side of the rock-water boundary at the bottom of the ocean are comp...
Similar Items
-
Advantages and challenges of tablet PC’s usage
by: Čičević Svetlana, et al.
Published: (2016-01-01) -
The character of the core-mantle boundary : a systematic study using PcP
by: Gassner, Alexandra Carina
Published: (2012) -
Observed travel times for Multiply-reflected ScS waves from a deep-focus earthquake
by: A. F. ESPISOSA
Published: (1966-06-01) -
Study of $$P_c(4457)$$ Pc(4457) , $$P_c(4440)$$ Pc(4440) , and $$P_c(4312)$$ Pc(4312) in a quasipotential Bethe–Salpeter equation approach
by: Jun He
Published: (2019-05-01) -
High Q ScS beneath the Ontong Java Plateau
by: Daisuke Suetsugu, et al.
Published: (2019-09-01)