Characterizing Holocene paleoseismic record in the SW Portuguense margin

Autor: Vizcaino A., E. Gracia, C. Escutia, A. Asioli, J. Garcia-Orellana: S. Lebreiro, I. Cacho, N. Thouveny, J.C. Larrasoana, S. Diez, J.J. Danobeitia

Publikováno v: EGU General Assembly 2006, Vienna, 2-7 Aprile 2006
info:cnr-pdr/source/autori:Vizcaino A.; E. Gracia; C. Escutia; A. Asioli; J. Garcia-Orellana: S. Lebreiro; I. Cacho; N. Thouveny; J.C. Larrasoana; S. Diez; J.J. Danobeitia/congresso_nome:EGU General Assembly 2006/congresso_luogo:Vienna/congresso_data:2-7 Aprile 2006/anno:2006/pagina_da:/pagina_a:/intervallo_pagine

The SW Iberian Margin is located at the convergence of the European and African Plates, where the largest magnitude earthquakes in Western Europe occur, such as the 1755 Lisbon event. Several active west-verging thrusts (i.e. Marquês de Pombal, São

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=cnr_________::c86f8518d3a5ccb6414261d1de2f36d5
http://www.cnr.it/prodotto/i/112121