Difference between revisions of "Dictionary:Fig R-3"
(Prepared the page for translation) |
(Marked this version for translation) |
||
Line 1: | Line 1: | ||
<languages/> | <languages/> | ||
<translate> | <translate> | ||
+ | <!--T:1--> | ||
[[File:Segr3.jpg|center]] | [[File:Segr3.jpg|center]] | ||
+ | <!--T:2--> | ||
FIG. R-3. | FIG. R-3. | ||
<b>Rayleigh-wave motion</b>. (<b>a</b>) Theoretical Rayleigh wave has retrograde elliptical motion at the surface. (<b>b</b>) Hodograph of particle velocity involved in ground roll. (From Howell, 1959, 80.) (<b>c</b>) Experimental measurements from a small explosion measured with buried geophones, showing the change from retrograde to prograde motion with depth. (After Dobrin, 1951). | <b>Rayleigh-wave motion</b>. (<b>a</b>) Theoretical Rayleigh wave has retrograde elliptical motion at the surface. (<b>b</b>) Hodograph of particle velocity involved in ground roll. (From Howell, 1959, 80.) (<b>c</b>) Experimental measurements from a small explosion measured with buried geophones, showing the change from retrograde to prograde motion with depth. (After Dobrin, 1951). | ||
</translate> | </translate> |
Latest revision as of 08:52, 27 May 2020
FIG. R-3. Rayleigh-wave motion. (a) Theoretical Rayleigh wave has retrograde elliptical motion at the surface. (b) Hodograph of particle velocity involved in ground roll. (From Howell, 1959, 80.) (c) Experimental measurements from a small explosion measured with buried geophones, showing the change from retrograde to prograde motion with depth. (After Dobrin, 1951).