Four shocks with epicenters in the region of the northern end of the Peninsular Range of Southern California were studied. Travel times of numerous phases of these four shocks were measured from seismograph records of stations at Pasadena, Mount Wilson, Riverside, La Jolla, Santa Barbara, Tinemaha and Haiwee, in Southern California. The velocities of propagation of eight principal phases were determined. Thicknesses of three layers above a depth of about 40 k.m. in the earth's crust were calculated
The travel times, periods, and amplitudes of SKP core waves have been investigated for shocks of nor...
Time terms resulting from an analysis of Pg seismic travel-time data from the Coast Ranges of centra...
The thickness and structure of the crust of the earth have been studied in a limited area of souther...
Four shocks with epicenters in the region of the northern end of the Peninsular Range of Southern Ca...
More than ten years ago the author published (Gutenberg, 1932) average travel-time curves for near-...
The system of seismological stations in California now makes it possible to study local shocks with ...
Discrepancies of up to 20 per cent between wave velocities calculated from blast records in southern...
The thickness and structure of the crust of the earth have been studied in a limited area of souther...
The present paper is a direct continuation of a recent paper (Gutenberg, 1944a) in which the author...
The present paper is a direct continuation of a recent paper (Gutenberg, 1944a) in which the author...
Recording of P and S at six or more stations to epicentral distances not over 160 km. makes it possi...
Recording of P and S at six or more stations to epicentral distances not over 160 km. makes it possi...
The travel times, periods, and amplitudes of SKP core waves have been investigated for shocks of nor...
A study has been made of the travel times of P waves as recorded from 14 shots on the Nevada Test Si...
The travel times, periods, and amplitudes of SKP core waves have been investigated for shocks of nor...
The travel times, periods, and amplitudes of SKP core waves have been investigated for shocks of nor...
Time terms resulting from an analysis of Pg seismic travel-time data from the Coast Ranges of centra...
The thickness and structure of the crust of the earth have been studied in a limited area of souther...
Four shocks with epicenters in the region of the northern end of the Peninsular Range of Southern Ca...
More than ten years ago the author published (Gutenberg, 1932) average travel-time curves for near-...
The system of seismological stations in California now makes it possible to study local shocks with ...
Discrepancies of up to 20 per cent between wave velocities calculated from blast records in southern...
The thickness and structure of the crust of the earth have been studied in a limited area of souther...
The present paper is a direct continuation of a recent paper (Gutenberg, 1944a) in which the author...
The present paper is a direct continuation of a recent paper (Gutenberg, 1944a) in which the author...
Recording of P and S at six or more stations to epicentral distances not over 160 km. makes it possi...
Recording of P and S at six or more stations to epicentral distances not over 160 km. makes it possi...
The travel times, periods, and amplitudes of SKP core waves have been investigated for shocks of nor...
A study has been made of the travel times of P waves as recorded from 14 shots on the Nevada Test Si...
The travel times, periods, and amplitudes of SKP core waves have been investigated for shocks of nor...
The travel times, periods, and amplitudes of SKP core waves have been investigated for shocks of nor...
Time terms resulting from an analysis of Pg seismic travel-time data from the Coast Ranges of centra...
The thickness and structure of the crust of the earth have been studied in a limited area of souther...