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- W78834815 abstract "Results obtained in the study of the arrival times of the Pn phase for the Friuli earthquake of 6 May 1976 (H = 20h00™15s,5; Normal 0 14 false false false MicrosoftInternetExplorer4 /* Style Definitions */ table.MsoNormalTable{mso-style-name:Tabella normale;mso-tstyle-rowband-size:0;mso-tstyle-colband-size:0;mso-style-noshow:yes;mso-style-parent:;mso-padding-alt:0pt 5.4pt 0pt 5.4pt;mso-para-margin:0pt;mso-para-margin-bottom:.0001pt;mso-pagination:widow-orphan;font-size:10.0pt;font-family:Times New Roman;mso-ansi-language:#0400;mso-fareast-language:#0400;mso-bidi-language:#0400;} φ = 46° 16'30 N; Normal 0 14 false false false MicrosoftInternetExplorer4 /* Style Definitions */ table.MsoNormalTable{mso-style-name:Tabella normale;mso-tstyle-rowband-size:0;mso-tstyle-colband-size:0;mso-style-noshow:yes;mso-style-parent:;mso-padding-alt:0pt 5.4pt 0pt 5.4pt;mso-para-margin:0pt;mso-para-margin-bottom:.0001pt;mso-pagination:widow-orphan;font-size:10.0pt;font-family:Times New Roman;mso-ansi-language:#0400;mso-fareast-language:#0400;mso-bidi-language:#0400;} λ = 13° 06' 00 E; M = 6.3) with respect to the epicentral distance are reported. Particular emphasis is given to the fact that the travel-time curves relative to the Pn waves and the corresponding equations are only valid for selected alignment. By plotting the time-distance curves it was possible to derive the depth of the lower surface of the upper mantle for different zones; the results thus obtained exibit significant differences." @default.
- W78834815 created "2016-06-24" @default.
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- W78834815 date "2010-05-26" @default.
- W78834815 modified "2023-09-29" @default.
- W78834815 title "On time-distance curves for Pn waves in the Friuli earthquake of 6 May 1976" @default.
- W78834815 doi "https://doi.org/10.4401/ag-4728" @default.
- W78834815 hasPublicationYear "2010" @default.
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