Matches in SemOpenAlex for { <https://semopenalex.org/work/W2548530909> ?p ?o ?g. }
Showing items 1 to 88 of
88
with 100 items per page.
- W2548530909 endingPage "249" @default.
- W2548530909 startingPage "237" @default.
- W2548530909 abstract "Abstract Two and a half years of data from an expanded, telemetered seismic network on the Olympic Peninsula reinforce the conclusion that the Juan de Fuca plate is subducting beneath Washington. However, the rate of seismicity is presently much lower than typical rates at other convergent margins. The located earthquakes can be divided into two groups on the basis of depth. At the coast, a shallow zone extends to a depth of approximately 20 km while a deep zone begins at 25 km. On the eastern edge of the Peninsula, the shallow zone has thickened to 30 km and the depth to the top of the deep zone has increased to 45 km. The rate of crustal seismicity is much lower on the Peninsula than in the adjacent Puget Sound region. The deep zone is 5 to 10 km thick and dips to the east at an angle of about 11°. The deep events appear to be occurring in the upper part of the subducting oceanic lithosphere. Focal mechanisms were constructed for 16 events in the suite of deep events with magnitudes ranging from 1.6 to 4.3. The solutions show primarily normal faulting with the P axes normal to the slab and the T axes displaying a range of angles within the slab with the average T axis in the downdip direction. Small events with down-dip tension in the downgoing slab are consistent with the slab sinking under its own weight. Several strike-slip events may be caused by a shearing within the slab. These features are consistent with ongoing subduction of the Juan de Fuca plate beneath North America." @default.
- W2548530909 created "2016-11-11" @default.
- W2548530909 creator A5008358584 @default.
- W2548530909 creator A5018078668 @default.
- W2548530909 date "1985-02-01" @default.
- W2548530909 modified "2023-10-14" @default.
- W2548530909 title "Seismicity and focal mechanisms associated with the subduction of the Juan de Fuca plate beneath the Olympic Peninsula, Washington" @default.
- W2548530909 cites W1545628673 @default.
- W2548530909 cites W1972567973 @default.
- W2548530909 cites W1987279793 @default.
- W2548530909 cites W1998796570 @default.
- W2548530909 cites W2024953052 @default.
- W2548530909 cites W2046227090 @default.
- W2548530909 cites W2059607962 @default.
- W2548530909 cites W2084273703 @default.
- W2548530909 cites W2086260649 @default.
- W2548530909 cites W2091733722 @default.
- W2548530909 cites W2098090725 @default.
- W2548530909 cites W2110693187 @default.
- W2548530909 cites W2126857433 @default.
- W2548530909 cites W2147716188 @default.
- W2548530909 cites W2157528639 @default.
- W2548530909 cites W2167273762 @default.
- W2548530909 cites W2168607185 @default.
- W2548530909 doi "https://doi.org/10.1785/bssa0750010237" @default.
- W2548530909 hasPublicationYear "1985" @default.
- W2548530909 type Work @default.
- W2548530909 sameAs 2548530909 @default.
- W2548530909 citedByCount "65" @default.
- W2548530909 countsByYear W25485309092012 @default.
- W2548530909 countsByYear W25485309092013 @default.
- W2548530909 countsByYear W25485309092015 @default.
- W2548530909 countsByYear W25485309092017 @default.
- W2548530909 countsByYear W25485309092020 @default.
- W2548530909 crossrefType "journal-article" @default.
- W2548530909 hasAuthorship W2548530909A5008358584 @default.
- W2548530909 hasAuthorship W2548530909A5018078668 @default.
- W2548530909 hasConcept C113740112 @default.
- W2548530909 hasConcept C119477230 @default.
- W2548530909 hasConcept C123588078 @default.
- W2548530909 hasConcept C127313418 @default.
- W2548530909 hasConcept C151730666 @default.
- W2548530909 hasConcept C165205528 @default.
- W2548530909 hasConcept C166957645 @default.
- W2548530909 hasConcept C16942324 @default.
- W2548530909 hasConcept C2777992645 @default.
- W2548530909 hasConcept C2777994876 @default.
- W2548530909 hasConcept C58097730 @default.
- W2548530909 hasConcept C77928131 @default.
- W2548530909 hasConcept C83176761 @default.
- W2548530909 hasConcept C95457728 @default.
- W2548530909 hasConcept C97490223 @default.
- W2548530909 hasConceptScore W2548530909C113740112 @default.
- W2548530909 hasConceptScore W2548530909C119477230 @default.
- W2548530909 hasConceptScore W2548530909C123588078 @default.
- W2548530909 hasConceptScore W2548530909C127313418 @default.
- W2548530909 hasConceptScore W2548530909C151730666 @default.
- W2548530909 hasConceptScore W2548530909C165205528 @default.
- W2548530909 hasConceptScore W2548530909C166957645 @default.
- W2548530909 hasConceptScore W2548530909C16942324 @default.
- W2548530909 hasConceptScore W2548530909C2777992645 @default.
- W2548530909 hasConceptScore W2548530909C2777994876 @default.
- W2548530909 hasConceptScore W2548530909C58097730 @default.
- W2548530909 hasConceptScore W2548530909C77928131 @default.
- W2548530909 hasConceptScore W2548530909C83176761 @default.
- W2548530909 hasConceptScore W2548530909C95457728 @default.
- W2548530909 hasConceptScore W2548530909C97490223 @default.
- W2548530909 hasIssue "1" @default.
- W2548530909 hasLocation W25485309091 @default.
- W2548530909 hasOpenAccess W2548530909 @default.
- W2548530909 hasPrimaryLocation W25485309091 @default.
- W2548530909 hasRelatedWork W1986164865 @default.
- W2548530909 hasRelatedWork W2045055260 @default.
- W2548530909 hasRelatedWork W2124535743 @default.
- W2548530909 hasRelatedWork W2259745315 @default.
- W2548530909 hasRelatedWork W2378286503 @default.
- W2548530909 hasRelatedWork W2790827251 @default.
- W2548530909 hasRelatedWork W2917235444 @default.
- W2548530909 hasRelatedWork W3087925122 @default.
- W2548530909 hasRelatedWork W4296617971 @default.
- W2548530909 hasRelatedWork W658779944 @default.
- W2548530909 hasVolume "75" @default.
- W2548530909 isParatext "false" @default.
- W2548530909 isRetracted "false" @default.
- W2548530909 magId "2548530909" @default.
- W2548530909 workType "article" @default.