About the focal mechanism of Friuli earthquake occurred on May 6, 1976

Summary We are going to present the focal-mechanism solution of Fruili earthquake occurred on May 6, 1976, as it results from the analysis, on original seismograms, of the polarities of initial longitudinal waves obtained in 92 seismic stations. The polarities so obtained have been reported on the p...
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Gespeichert in:

Autor*in:	Biagi, P. F. [verfasserIn] Piro, S.

Format:	Artikel
Sprache:	Englisch

Erschienen:	1980

Schlagwörter:	Focal Mechanism Focal Depth Nodal Plane Nodal Line Dallo

Anmerkung:	© Società Italiana di Fisica 1980

Übergeordnetes Werk:	Enthalten in: Il Nuovo Cimento C - Kluwer Academic Publishers, 1978, 3(1980), 2 vom: März, Seite 142-150
Übergeordnetes Werk:	volume:3 ; year:1980 ; number:2 ; month:03 ; pages:142-150

Links:	Volltext

DOI / URN:	10.1007/BF02507140

Katalog-ID:	OLC2055363352

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650		4	\|a Focal Mechanism
650		4	\|a Focal Depth
650		4	\|a Nodal Plane
650		4	\|a Nodal Line
650		4	\|a Dallo
700	1		\|a Piro, S. \|4 aut
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title_sort	about the focal mechanism of friuli earthquake occurred on may 6, 1976
title_auth	About the focal mechanism of Friuli earthquake occurred on May 6, 1976
abstract	Summary We are going to present the focal-mechanism solution of Fruili earthquake occurred on May 6, 1976, as it results from the analysis, on original seismograms, of the polarities of initial longitudinal waves obtained in 92 seismic stations. The polarities so obtained have been reported on the projection which represents the surface of the Earth and the solution has been drawn, directly, from the study of the resulting distribution, by establishing through Gräfe's theory the two couples of forces considered as the sources of the seism at the focus. At last, a comparison has been carried out with the solution already obtained by other authors. © Società Italiana di Fisica 1980
abstractGer	Summary We are going to present the focal-mechanism solution of Fruili earthquake occurred on May 6, 1976, as it results from the analysis, on original seismograms, of the polarities of initial longitudinal waves obtained in 92 seismic stations. The polarities so obtained have been reported on the projection which represents the surface of the Earth and the solution has been drawn, directly, from the study of the resulting distribution, by establishing through Gräfe's theory the two couples of forces considered as the sources of the seism at the focus. At last, a comparison has been carried out with the solution already obtained by other authors. © Società Italiana di Fisica 1980
abstract_unstemmed	Summary We are going to present the focal-mechanism solution of Fruili earthquake occurred on May 6, 1976, as it results from the analysis, on original seismograms, of the polarities of initial longitudinal waves obtained in 92 seismic stations. The polarities so obtained have been reported on the projection which represents the surface of the Earth and the solution has been drawn, directly, from the study of the resulting distribution, by establishing through Gräfe's theory the two couples of forces considered as the sources of the seism at the focus. At last, a comparison has been carried out with the solution already obtained by other authors. © Società Italiana di Fisica 1980
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title_short	About the focal mechanism of Friuli earthquake occurred on May 6, 1976
url	https://doi.org/10.1007/BF02507140
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author2	Piro, S.
author2Str	Piro, S.
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doi_str	10.1007/BF02507140
up_date	2024-07-04T02:01:38.678Z
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