Amount of subsidence during a late Holocene earthquake—evidence from fossil tidal marsh foraminifera at Vancouver Island, west coast of Canada
- 1 October 1995
- journal article
- Published by Elsevier in Palaeogeography, Palaeoclimatology, Palaeoecology
- Vol. 118 (1-2) , 49-71
- https://doi.org/10.1016/0031-0182(94)00135-u
Abstract
No abstract availableKeywords
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