P-wave deep velocity structure of the Southern Tyrrhenian Subduction Zone from nonlinear teleseismic traveltime tomography

A new 3‐D model for the P‐wave velocity structure of the Southern Tyrrhenian Subduction Zone (STSZ) is determined from nonlinear inversion of relative arrival times of teleseismic events. The data used in the imaging are the travel time residuals of both direct, P and PKPdf and secondary pP, sP, PcP...

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Veröffentlicht in:	Geophysical research letters 1999-12, Vol.26 (24), p.3709-3712
1. Verfasser:	Cimini, Giovanni B.
Format:	Artikel
Sprache:	eng
Schlagworte:	Earth sciences Earth, ocean, space Exact sciences and technology Tectonics. Structural geology. Plate tectonics
Online-Zugang:	Volltext
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