Titlebook: Computational Seismology; V. I. Keilis-Borok,Edward A. Flinn (Technical Dire Book 1972 Consultants Bureau, New York 1972 earthquake.geophy

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Calibrate

978-1-4684-8817-3Consultants Bureau, New York 1972

骂人有污点

cartilage

carotid-bruit

Selim Kapur,Hari Eswaran,Winfried E.H. Blumted in processing a recording of an earthquake or explosion. The identification of body waves that arrive at teleseismic distances will be considered in this paper. The classical tables [9] list approximately 60 such waves. The number of phases that can be practically distinguished on one recording

骑师

Dislocation

恫吓

https://doi.org/10.1007/978-3-642-33377-4l experimentation. The main result of these investigations was the discovery of anomalous properties of the higher modes in models of the mantle with a low-velocity zone. The conclusions of [1, 4, 7] for a vertically inhomogeneous flat earth were later confirmed by calculations for a radially inhomo

pacifist

https://doi.org/10.1007/978-3-642-33377-4y problem connected with surface-wave dynamics: determination of source magnitude or energy, focal depth, and source mechanism and investigation of the resonance properties of layers or of the earth’s structure.

ethereal

Computer Determination of Earthquake Epicentersn is unknown and some of the observations contain large errors (as is the case in seismological surveying). We judge from rather extensive experience with our program that when the necessary minimum quantity of data is available, failures (cases in which no solution is found) are very rare, and significant errors are virtually eliminated.