FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2103819921> ?p ?o ?g. }

• W2103819921 endingPage "4134" @default.
• W2103819921 startingPage "4129" @default.
• W2103819921 abstract "The composition and elastic properties of the earth's lithosphere beneath the sea floor are fundamental to our understanding of the mechanism of sea floor spreading and continental drift. New experimental information on the elastic properties, as a function of temperature, pressure, and petrology, of eclogite and peridotite is presented. The density and seismic wave velocities in peridotite simulated in the laboratory for the oceanic lithosphere of the first 15–20 km of depth match results of recent seismic investigations very well. The elastic properties of olivine eclogite describe the seismic structure of the remaining lithosphere. The present study favors the idea of a chemical change within the lithosphere, and our laboratory results tend to favor ∼22 for the oceanic lithosphere. In modeling the structure in terms of temperature and pressure coefficients the surface wave studies introduce two complications: First, since partial melting is required by the very low shear wave velocities of the asthenosphere, some consistent and sensible way of treating velocities in mush must be used. Second, the mantle is anisotropic; therefore a systematic crystal orientation has to be considered rather than just the average Vp and Vs for the mantle constituents. The seismic anomalies of azimuth-dependent fluctuations in the velocity of Pn waves along the base of the oceanic crust are as much as 8%; the high velocity tends to be in the direction of sea floor spreading. A consistent explanation of this effect would be the presence of a sustained extensional strain rate in the spreading direction, applied at the base of the oceanic lithosphere. It would appear that the anisotropy vanishes near the surface of the oceanic plate." @default.
• W2103819921 created "2016-06-24" @default.
• W2103819921 creator A5044998099 @default.
• W2103819921 date "1976-08-10" @default.
• W2103819921 modified "2023-10-17" @default.
• W2103819921 title "On the composition of the oceanic lithosphere" @default.
• W2103819921 cites W1974029863 @default.
• W2103819921 cites W1987098602 @default.
• W2103819921 cites W1987194631 @default.
• W2103819921 cites W1992915876 @default.
• W2103819921 cites W1997911623 @default.
• W2103819921 cites W1999584382 @default.
• W2103819921 cites W2001823899 @default.
• W2103819921 cites W2005004607 @default.
• W2103819921 cites W2024732062 @default.
• W2103819921 cites W2043676912 @default.
• W2103819921 cites W2045041750 @default.
• W2103819921 cites W2061388996 @default.
• W2103819921 cites W2062490754 @default.
• W2103819921 cites W2069477573 @default.
• W2103819921 cites W2069743827 @default.
• W2103819921 cites W2074037274 @default.
• W2103819921 cites W2106781958 @default.
• W2103819921 cites W2125186533 @default.
• W2103819921 cites W2136433737 @default.
• W2103819921 cites W2142573992 @default.
• W2103819921 cites W2148348970 @default.
• W2103819921 cites W2165258323 @default.
• W2103819921 cites W2166026905 @default.
• W2103819921 cites W2246718442 @default.
• W2103819921 cites W2764955449 @default.
• W2103819921 doi "https://doi.org/10.1029/jb081i023p04129" @default.
• W2103819921 hasPublicationYear "1976" @default.
• W2103819921 type Work @default.
• W2103819921 sameAs 2103819921 @default.
• W2103819921 citedByCount "7" @default.
• W2103819921 crossrefType "journal-article" @default.
• W2103819921 hasAuthorship W2103819921A5044998099 @default.
• W2103819921 hasConcept C127313418 @default.
• W2103819921 hasConcept C13495919 @default.
• W2103819921 hasConcept C154200439 @default.
• W2103819921 hasConcept C162075064 @default.
• W2103819921 hasConcept C165205528 @default.
• W2103819921 hasConcept C16942324 @default.
• W2103819921 hasConcept C173347748 @default.
• W2103819921 hasConcept C23148476 @default.
• W2103819921 hasConcept C2776698055 @default.
• W2103819921 hasConcept C58097730 @default.
• W2103819921 hasConcept C5900021 @default.
• W2103819921 hasConcept C67236022 @default.
• W2103819921 hasConcept C77928131 @default.
• W2103819921 hasConcept C8058405 @default.
• W2103819921 hasConcept C84372278 @default.
• W2103819921 hasConceptScore W2103819921C127313418 @default.
• W2103819921 hasConceptScore W2103819921C13495919 @default.
• W2103819921 hasConceptScore W2103819921C154200439 @default.
• W2103819921 hasConceptScore W2103819921C162075064 @default.
• W2103819921 hasConceptScore W2103819921C165205528 @default.
• W2103819921 hasConceptScore W2103819921C16942324 @default.
• W2103819921 hasConceptScore W2103819921C173347748 @default.
• W2103819921 hasConceptScore W2103819921C23148476 @default.
• W2103819921 hasConceptScore W2103819921C2776698055 @default.
• W2103819921 hasConceptScore W2103819921C58097730 @default.
• W2103819921 hasConceptScore W2103819921C5900021 @default.
• W2103819921 hasConceptScore W2103819921C67236022 @default.
• W2103819921 hasConceptScore W2103819921C77928131 @default.
• W2103819921 hasConceptScore W2103819921C8058405 @default.
• W2103819921 hasConceptScore W2103819921C84372278 @default.
• W2103819921 hasIssue "23" @default.
• W2103819921 hasLocation W21038199211 @default.
• W2103819921 hasOpenAccess W2103819921 @default.
• W2103819921 hasPrimaryLocation W21038199211 @default.
• W2103819921 hasRelatedWork W1990568759 @default.
• W2103819921 hasRelatedWork W2022784417 @default.
• W2103819921 hasRelatedWork W2061740219 @default.
• W2103819921 hasRelatedWork W2083883565 @default.
• W2103819921 hasRelatedWork W2103819921 @default.
• W2103819921 hasRelatedWork W2764447590 @default.
• W2103819921 hasRelatedWork W2990888247 @default.
• W2103819921 hasRelatedWork W3095318176 @default.
• W2103819921 hasRelatedWork W4251301102 @default.
• W2103819921 hasRelatedWork W93469224 @default.
• W2103819921 hasVolume "81" @default.
• W2103819921 isParatext "false" @default.
• W2103819921 isRetracted "false" @default.
• W2103819921 magId "2103819921" @default.
• W2103819921 workType "article" @default.