Determination of magnitude for Kurile-Kamchatka earthquakes

Solovyev, S. L.; Solovyeva, O. N.

doi:10.1007/bf02587846

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Such a Behaviour Of 5 Is Obvious From Figs 3(a) And (B)1

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“…(b) Analysis of the relation of maximal values of oscillation velocity in body and surface waves is given on the basis of the determination of mpv and M L H . Dependence between mpv and M,, as a function of depth was given in a paper by Soloviev & Solovieva (1962). According to this dependence a mean depth has proved to be of 6Ok 15 km.…”

Section: Such a Behaviour Of 5 Is Obvious From Figs 3(a) And (B)mentioning

confidence: 87%

On the Determination of the Extent of an Indian Shock Origin by Kinematic Data

Gorbunova

Kondorskaya

Landyreva

1970

Geophysical Journal International

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Results of instrumental observations of the Koyna earthquake of 1967 December 10 have been generalized in this paper.First arrival times of seismic waves recorded in the distance range of 0.03" to loo" have been used. A set of origin locations has been found from different samples of the seismic observations. The data obtained suggest the origin extension as being 20-25 km in the horizontal direction and 60-80 km in the vertical one. The limits of the focal region have been fixed by systems of near and teleseismic stations.Dynamic parameters of seismic waves at teleseismic stations give evidence of radiation from a deep source.

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Section: Such a Behaviour Of 5 Is Obvious From Figs 3(a) And (B)mentioning

confidence: 87%