New constraints on coseismic slip during southern Cascadia subduction zone earthquakes over the past 4600 years implied by tsunami deposits and marine turbidites

Authors

GR Priest
RC Witter
Yinglong J. Zhang, Virginia Institute of Marine ScienceFollow
C Goldfinger
KL Wang
JC Allen

Document Type

Article

Department/Program

Virginia Institute of Marine Science

Publication Date

2018

Journal

Natural Hazards

Volume

93

Issue

2

First Page

1109

Last Page

1111

Abstract

This correction stands to correct Figure 7c listing a low minimum slip of 12 m for Case 2 instead of the correct value of 8 m, as stated in the body of the text and depicted on the chart of cumulative slip. The corrected chart explanation and caption are shown below. This error did not affect any of the findings of the paper or the chart itself. This is a correction to the original article.

DOI

10.1007/s11069-018-3405-x

Recommended Citation

Priest, GR; Witter, RC; Zhang, Yinglong J.; Goldfinger, C; Wang, KL; and Allen, JC, New constraints on coseismic slip during southern Cascadia subduction zone earthquakes over the past 4600 years implied by tsunami deposits and marine turbidites (2018). Natural Hazards, 93(2), 1109-1111.

10.1007/s11069-018-3405-x