In:
Journal of Geophysical Research: Solid Earth, American Geophysical Union (AGU), Vol. 124, No. 8 ( 2019-08), p. 7538-7561
Abstract:
The 1929 Grand Banks tsunamigenic landslide included a massive slump and not just surficial landslides as described in earlier literature The slump (~500‐m thick) occurred along oblique faults (~17°) with vertical offsets of 100 m and horizontal offsets of 330 m Both the massive slump (~560 km³) and translational surficial (upper 20 m) sediment failures likely contributed to the 1929 tsunami
Type of Medium:
Online Resource
ISSN:
2169-9313
,
2169-9356
DOI:
10.1029/2018JB017066
Language:
English
Publisher:
American Geophysical Union (AGU)
Publication Date:
2019
detail.hit.zdb_id:
2016813-5
detail.hit.zdb_id:
161666-3
detail.hit.zdb_id:
3094197-0
SSG:
16,13
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