 | 1967 - عدد الصفحات: 650
...anomalie« and their Interpretation [AFCRL-67-0285] 19 р343в N87-32806 An analysis of the travel time» of S waves to North American stations, In the distance range 28 deg to 81 deg [AFCRL-e7-0284] 19 p3437 N87-32809 RALES. KA Minimum-fuel attitude control of t rUld... | |
 | 1970 - عدد الصفحات: 1096
...project: Los Angeles County Mus. Nat. History Quart., v. 6, no. 1 , p. 20-25, illus.. 1 967. 03005 Doyle, HA; Hales, AL An analysis of the travel times...82°: Seismol. Soc. America Bull., v. 57. no. 4. p. 76 1-771, illus., tables, 1 967. Doyle, HA See Hales. AL 04347 0451 1 Doyle, Larry .1.: Maynard, J.... | |
 | 1968 - عدد الصفحات: 978
...a low line. This method of transportation prevented breaking of the many small bones.— ESL 03005 Doyle, HA; Hales, AL An analysis of the travel times...82°: Seismol. Soc. America Bull.. v. 57, no. 4, p. 761 771, illus., tables, 1967. S-wave traveltimes from 20 earthquakes to North American stations at... | |
 | Ian Jackson - 2000 - عدد الصفحات: 600
...P'P' re-examined using broad-band data. Geophys. J. Int. 99:595-604. Doyle, HA, and Hales, AL 1967. An analysis of the travel times of S waves to North...American stations, in the distance range 28° to 82°. Bull. Seismol. Soc. Am. 57:761-71. Duffy, TS, and Anderson, DL 1989. Seismic velocities in mantle minerals... | |
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An analysis of the travel times of S waves to North American stations, in the distance range 28° to 82°, Bull• seism. 