On the data integration of seismological observation and deep seismic exploration. The crustal modeling for the Messina Straits Area as an example

Given an earth crust model having homogeneous layers and sphericalsymmetry, the travel-times equations of the direct and refracted longitudinalwaves are first deduced. These linear equations are determinedfrom the seismic ray parameter p, and from the known term a,. Theparameter p, is connected with...

詳細記述

書誌詳細

出版年:	Annals of Geophysics
主要な著者:	Antonio Bottari, B. Federico
フォーマット:	論文
言語:	英語
出版事項:	National Institute of Geophysics and Volcanology 2010
主題:	Seismic Waves and Analysis Seismic Imaging and Inversion Techniques earthquake and tectonic studies Strait of Messina seismic data integration deep seismic exploration first arrival time crustal velocity structure
オンライン･アクセス:	https://doi.org/10.4401/ag-4689
タグ:	タグ追加 タグなし, このレコードへの初めてのタグを付けませんか!