@article {Weirathmueller2017a,
	title = {Spatial and temporal trends in fin whale vocalizations recorded in the NE Pacific Ocean between 2003-2013},
	journal = {PLOS ONE},
	volume = {12},
	number = {10},
	year = {2017},
	month = {oct},
	pages = {e0186127},
	issn = {1932-6203},
	doi = {10.1371/journal.pone.0186127},
	url = {https://dx.plos.org/10.1371/journal.pone.0186127},
	author = {Weirathmueller, Michelle J. and Stafford, Kathleen M. and Wilcock, William S. D. and Hilmo, Rose S. and Dziak, Robert P. and Tr{\'e}hu, Anne M.},
	editor = {Li, Songhai}
}
@article {williams_seismicity_2011,
	title = {Seismicity at the Cascadia Plate Boundary beneath the Oregon Continental Shelf},
	journal = {Bulletin of the Seismological Society of America},
	volume = {101},
	number = {3},
	year = {2011},
	pages = {940{\textendash}950},
	abstract = {Since 2003, 39 small earthquakes have been detected off the coast of central Oregon in the nominally locked part of the Cascadia subduction zone, where very little seismic activity has been recorded in spite of a paleoseismic record of great subduction events. Although the regional earthquake bulletin reports depths of 29 and 28~km for the two largest events (Mw~4.9 and Mw~4.7, which occurred in 2004), analysis by Tr{\'e}hu et~al. (2008) indicates that they were low-angle thrust events that occurred on the plate boundary at depths of 9{\textendash}11 and 16~km, respectively. Because of sparse onshore station coverage, most of the smaller events have large location uncertainties. Double-difference relative location of 30 of these earthquakes reveals two tight clusters approximately 30~km apart; each cluster is associated with one of the two larger events. Within each cluster, relocation reduces the hypocenter depth spread from \&gt;15 km to \&lt;3 km, with uncertainties on the order of 0.1~km. The relocations, combined with independent absolute hypocenter locations for two 2008 events using a deployment of land and ocean-bottom seismometers, suggest that the seismicity occurred at plate boundary depths, possibly on the Cascadia megathrust. This concentrated activity in the seismogenic zone may represent patches on the fault plane with anomalous frictional characteristics, possibly caused by subducted topographic features, which can affect the propagation of a large megathrust rupture.},
	issn = {0037-1106},
	doi = {10.1785/0120100198},
	url = {https://doi.org/10.1785/0120100198},
	author = {Williams, Mark C. and Tr{\'e}hu, Anne M. and Braunmiller, Jochen}
}
