An inverse problem in seismology: derivation of the seismic source parameters from P and S seismic waves

Author:

Apostol Bogdan FelixORCID

Funder

Scientific Education and Research Institute

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology,Geophysics

Reference39 articles.

1. Aki K (1966) Generation and propagation of G waves from the Niigata earthquake of June 16, 1964. 2. Estimation of earthquake movement, relased energy, and stress-strain drop from G wave spectrum. Bull Earthquake Res Inst Tokyo Univ 44:23–88

2. Aki K, Richards PG (2009) Quantitative seismology. University Science Books, Sausalito

3. Apostol BF (2017a) Elastic waves inside and on the surface of a half-space. Quart J Mech Appl Math 70:289–308

4. Apostol BF (2017b) Elastic displacement in a half-space under the action of a tensor force. General solution for the half-space with point forces. J Elast 126:231–244

5. Arvidsson R, Ekstrom G (1998) Global CMT analysis of moderate earthquakes, $M_{w}\geqq 4.5$, using intermediate-period surface waves. Bull Seism Soc Am 88:1003–1013

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