Large-Scale Fluidization Features from Late Holocene Coseismic Paleoliquefaction in the Willamette River Forearc Valley, Central Cascadia Subduction Zone, Oregon, USA

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ISSN Print: 2169-9623
ISSN Online: 2169-9631
www.scirp.org/journal/ojer
E-mail: ojer@scirp.org

"Large-Scale Fluidization Features from Late Holocene Coseismic Paleoliquefaction in the Willamette River Forearc Valley, Central Cascadia Subduction Zone, Oregon, USA"
written by Curt D. Peterson, Kurt Kristensen, Rick Minor,
published by Open Journal of Earthquake Research, Vol.3 No.2, 2014

has been cited by the following article(s):

[1]	Decoding Seismic Hazard Enigmas via Next-Generation Paleoseismic Analyses: With Application to the Cascadia Subduction Zone and Beyond
	2023

[2]	Cascadia Earthquake-Triggered Rockslide Burial of Beeswax Galleon Wreck Timbers in a Sea Cliff Wave-Cut Platform Site, North Smuggler Cove, Oregon, USA
	Journal of Geography and …, 2023

[3]	Compilation and forecasting of paleoliquefaction evidence for the strength of ground motions in the US Pacific Northwest
	2021

[4]	Cascadia Convergent Zone: An Example of Primary Convergent Seismogenic Structure
	2019

[5]	Late Stage Interseismic Strain Interval, Cascadia Subduction Zone Margin, USA and Canada
	2017

[6]	Towards a national map of soil liquefaction susceptibility: modeling with heuristic and geotechnical methods
	2014

[1]	Implications of physics-based M9 ground motions on liquefaction-induced damage in the Cascadia Subduction Zone: Looking forward and backward Earthquake Spectra, 2025 DOI:10.1177/87552930251316819

[2]	Compilation and forecasting of paleoliquefaction evidence for the strength of ground motions in the U.S. Pacific Northwest Engineering Geology, 2021 DOI:10.1016/j.enggeo.2021.106253

[3]	Compilation and forecasting of paleoliquefaction evidence for the strength of ground motions in the U.S. Pacific Northwest Engineering Geology, 2021 DOI:10.1016/j.enggeo.2021.106253

[4]	Late Stage Interseismic Strain Interval, Cascadia Subduction Zone Margin, USA and Canada Open Journal of Earthquake Research, 2017 DOI:10.4236/ojer.2017.61001

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