@article {morton_newly_2018,
	title = {Newly detected earthquakes in the Cascadia subduction zone linked to seamount subduction and deformed upper plate},
	journal = {Geology},
	volume = {46},
	number = {11},
	year = {2018},
	month = {09/2018},
	pages = {943{\textendash}946},
	abstract = {Data from an amphibious seismic network in Cascadia (northwest North America) provide unique near-source observations to assess the influence of subducting topography on seismicity. Using subspace detection, we detect and locate 222 events in two separate clusters, near a subducted seamount and a possibly accreted seamount. Seismicity in both clusters is largely shallower than the plate interface and exhibits occasional swarm-like behavior. This implies that the seamount is subducting aseismically via weak coupling with the overriding plate, while earthquakes in the upper plate arise from a high degree of fracturing due to seamount interaction, and the accreted seamount induced similar fracturing before off-scraping.},
	issn = {0091-7613},
	doi = {10.1130/G45354.1},
	url = {https://doi.org/10.1130/G45354.1},
	author = {Morton, Emily A. and Bilek, Susan L. and Rowe, Charlotte A.}
}
