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Volume 13, issue 8 | Copyright

Special issue: Marine and lake paleoseismology

Nat. Hazards Earth Syst. Sci., 13, 2109-2146, 2013
https://doi.org/10.5194/nhess-13-2109-2013
© Author(s) 2013. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 23 Aug 2013

Research article | 23 Aug 2013

Spatially limited mud turbidites on the Cascadia margin: segmented earthquake ruptures?

C. Goldfinger et al.
Cited articles
Abdeldayem, A. L., Ikehara, K., and Yamazaki, T.: Flow path of the 1993 Hokkaido-Nansei-oki earthquake seismoturbidite, southern margin of the Japan sea north basin, inferred from anisotropy of magnetic susceptibility: Geophys. J. Int., 157, 15–24, 2004.
Abrams, L. J.: Correlation among core, logging, and seismic data at Site 1149 in the Nadezhda Basin, edited by: Ludden, J. N., Plank, T., and Escutia, C., Proc. ODP, Sci. Results, 185, available at: http://www-odp.tamu.edu/publications/185_SR/001/001.htm (last access: 9 September 2012), 2002.
Adams, J.: Paleoseismicity of the Cascadia subduction zone: evidence from turbidites off the Oregon-Washington margin, Tectonics, 9, 569–583, 1990.
Anastasakis, G. C. and Piper, D. J. W.: The character of seismo-turbidites in the S-1 sapropel, Zakinthos and Strofadhes basins, Greece, Sedimentology, 38, 717–733, 1991.
Awadallah, S. A. M.: Fine-grained turbidites of the Amazon Fan: facies characterization and interpretation, edited by: Taylor, B. and Klaus, A., Proc. ODP, Sci. Results, 180, 1–30, 2001.
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