S. Lorito (1), F. Romano (1), S. Atzori (1), X. Tong (2), A. Avallone (1), J. McCloskey (3), M. Cocco (1), E. Boschi (1) and A. Piatanesi (1)
(1) Istituto Nazionale di Geofisica e Vulcanologia, Italy
(2) Institute of Geophysics and Planetary Physics, Scripps Institution of Oceanography, University of California, San Diego,
La Jolla, California 92093-0225, USA
(3) Environmental Sciences Research Institute, School of Environmental Sciences, University of Ulster, Coleraine BT52 1SA,
Northern Ireland
Tale articolo ? stato pubblicato recentemente su Nature Geoscience e ricostruisce la rottura durante il grande terremoto del 27 Febbraio 2010 in Cile e ne discute le implicazioni per i grandi terremoti di subduzione.
Didascalia figura - Slip distribution for the 2010 Mw 8.8 Maule earthquake, compared with the estimated position of the Darwin gap, in the segment where the 1835 earthquake probably occurred. White arrows represent the slip direction (rake). Thin black contours indicate the associated surface vertical displacement (1-m-interval solid lines for uplift, 20-cm-interval dashed lines for subsidence).
Segnaliamo inoltre la registrazione commentata da Stefano Lorito sul canale
Lorito S. et alii (2011) - Limited overlap between the seismic gap and coseismic slip of the great 2010 Chile earthquake.
Nature Geoscience, vol. 4, 173–177 (2011). doi:10.1038/ngeo1073