High tsunami frequency as a result of combined strike-slip faulting and coastal landslides-Reference-Cited by-同舟云学术

High tsunami frequency as a result of combined strike-slip faulting and coastal landslides

Published:2010-10-10 Issue:11 Volume:3 Page:783-788
ISSN:1752-0894
Container-title:Nature Geoscience
language:en
Short-container-title:Nature Geosci

Author:

Hornbach Matthew J.,Braudy Nicole,Briggs Richard W.,Cormier Marie-Helene,Davis Marcy B.,Diebold John B.,Dieudonne Nicole,Douilly Roby,Frohlich Cliff,Gulick Sean P. S.,Johnson III Harold E.,Mann Paul,McHugh Cecilia,Ryan-Mishkin Katherine,Prentice Carol S.,Seeber Leonardo,Sorlien Christopher C.,Steckler Michael S.,Symithe Steeve Julien,Taylor Frederick W.,Templeton John

Publisher

Springer Science and Business Media LLC

Subject

General Earth and Planetary Sciences

Link

http://www.nature.com/articles/ngeo975.pdf

Reference32 articles.

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2. Yalçıner, A. C., Alpar, B., Altınok, Y., Özbay, I. & Imamura, F. Tsunamis in the Sea of Marmara: Historical documents for the past, models for the future. Mar. Geol. 15, 445–463 (2002).

3. Segall, P. & Lisowski, M. Surface displacements in the 1906 San Francisco and 1989 Loma Prieta earthquakes. Science 250, 1241–1244 (1990).

4. Tinti, S. et al. The generation mechanisms of the August 17, 1999 Izmit bay (Turkey) tsunami: Regional (tectonic) and local (mass instabilities) causes. Mar. Geol. 225, 311–330 (2006).

5. Heck, N. H. List of seismic sea waves. Bull. Seismol. Soc. Am. 37, 269–286 (1947).

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