FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W1965158002> ?p ?o ?g. }

• W1965158002 endingPage "4371" @default.
• W1965158002 startingPage "4359" @default.
• W1965158002 abstract "The elastic moduli of a synthetic single crystal of pure FeSiO 3 , orthoferrosilite, have been measured at 1 bar and 20°C by Brillouin spectroscopy. The moduli are (in megabars) c 11 = 1.98, c 22 = 1.36, c 33 = 1.75, c 44 = 0.59, c 55 = 0.58, c 66 = 0.49, c 12 = 0.84, c 13 = 0.72, c 23 = 0.55. A comparison of the pyroxene crystal structure with elasticity data shows that distortion of the tetrahedral chains parallel to c is related to c 33 Straight or extended chains increase c 33 , and highly kinked chains weaken the structure. However, the ferrosilite data show that beyond a certain degree of distortion the tetrahedral chains are essentially passive. Previous models of pyroxene elasticity have indicated that c 11 should be most sensitive to composition. This is supported by the current study and is reflected in the elasticity data via a positive linear correlation of c 11 with the size of the M1 octahedron, as measured by the average M1‐0 distance. The average longitudinal modulus 11 ((c 11 + c 22 + c 33 )/3) varies linearly with composition in the system orthoenstatite‐orthoferrosilite, whereas the average shear moduli ¯ 44 and ¯ 12 are constant for Fe contents of at least 20%. By comparison, data for the solid solution forsterite‐fayalite are consistent with a linear variation of modulus versus composition between the end‐members for all three average moduli. We suggest that this difference between orthopyroxene and olivine is due to a strong preference of Fe 2+ for the M2 octahedral site in pyroxene. The isotropic shear modulus μ is 30% lower for ferrosilite than enstatite. Despite a similar contrast in end‐member values of μ, the olivine data are consistent with a linear variation of μ between Fo 100 and Fa 100 . At high temperatures, Fe and Mg in orthopyroxene will be randomly distributed, and a linear variation of μ with molar content of Fe is expected. A comparison of laboratory elasticity data with observed mantle properties shows that V p , V s , and ρ of the upper mantle are satisfied by pure olivine. However, the data strongly suggest that without the coexistence of a garnet phase, no more than 10% orthopyroxene may be present in a model mantle assemblage. Ca‐clinopyroxene increases the upper limit on mantle garnet content but does not greatly affect constraints on the quantity of orthopyroxene in the upper mantle." @default.
• W1965158002 created "2016-06-24" @default.
• W1965158002 creator A5066967648 @default.
• W1965158002 creator A5081074565 @default.
• W1965158002 date "1984-06-10" @default.
• W1965158002 modified "2023-10-13" @default.
• W1965158002 title "Elasticity of single‐crystal orthoferrosilite" @default.
• W1965158002 cites W1524374098 @default.
• W1965158002 cites W1965512089 @default.
• W1965158002 cites W1967402452 @default.
• W1965158002 cites W1984639573 @default.
• W1965158002 cites W1988895990 @default.
• W1965158002 cites W1993793225 @default.
• W1965158002 cites W1994414709 @default.
• W1965158002 cites W2009896114 @default.
• W1965158002 cites W2015941464 @default.
• W1965158002 cites W2016409790 @default.
• W1965158002 cites W2022328899 @default.
• W1965158002 cites W2022479559 @default.
• W1965158002 cites W2028130517 @default.
• W1965158002 cites W2035730164 @default.
• W1965158002 cites W2039657115 @default.
• W1965158002 cites W2047037925 @default.
• W1965158002 cites W2047045913 @default.
• W1965158002 cites W2055272486 @default.
• W1965158002 cites W2056835616 @default.
• W1965158002 cites W2062221814 @default.
• W1965158002 cites W2066070963 @default.
• W1965158002 cites W2073040485 @default.
• W1965158002 cites W2075908582 @default.
• W1965158002 cites W2086807579 @default.
• W1965158002 cites W2086811113 @default.
• W1965158002 cites W2094704767 @default.
• W1965158002 cites W2106955797 @default.
• W1965158002 cites W2110427390 @default.
• W1965158002 cites W2123419464 @default.
• W1965158002 cites W2131551151 @default.
• W1965158002 cites W2169452944 @default.
• W1965158002 cites W2180899245 @default.
• W1965158002 cites W2494825342 @default.
• W1965158002 cites W2900255971 @default.
• W1965158002 doi "https://doi.org/10.1029/jb089ib06p04359" @default.
• W1965158002 hasPublicationYear "1984" @default.
• W1965158002 type Work @default.
• W1965158002 sameAs 1965158002 @default.
• W1965158002 citedByCount "153" @default.
• W1965158002 countsByYear W19651580022012 @default.
• W1965158002 countsByYear W19651580022013 @default.
• W1965158002 countsByYear W19651580022014 @default.
• W1965158002 countsByYear W19651580022015 @default.
• W1965158002 countsByYear W19651580022016 @default.
• W1965158002 countsByYear W19651580022017 @default.
• W1965158002 countsByYear W19651580022018 @default.
• W1965158002 countsByYear W19651580022019 @default.
• W1965158002 countsByYear W19651580022020 @default.
• W1965158002 countsByYear W19651580022022 @default.
• W1965158002 crossrefType "journal-article" @default.
• W1965158002 hasAuthorship W1965158002A5066967648 @default.
• W1965158002 hasAuthorship W1965158002A5081074565 @default.
• W1965158002 hasConcept C115624301 @default.
• W1965158002 hasConcept C120665830 @default.
• W1965158002 hasConcept C121089165 @default.
• W1965158002 hasConcept C121332964 @default.
• W1965158002 hasConcept C121854251 @default.
• W1965158002 hasConcept C159985019 @default.
• W1965158002 hasConcept C185592680 @default.
• W1965158002 hasConcept C192562407 @default.
• W1965158002 hasConcept C194232370 @default.
• W1965158002 hasConcept C198819137 @default.
• W1965158002 hasConcept C199289684 @default.
• W1965158002 hasConcept C2777554867 @default.
• W1965158002 hasConcept C2778189432 @default.
• W1965158002 hasConcept C2778998827 @default.
• W1965158002 hasConcept C2780364934 @default.
• W1965158002 hasConcept C2781137303 @default.
• W1965158002 hasConcept C41279357 @default.
• W1965158002 hasConcept C43486711 @default.
• W1965158002 hasConcept C43989790 @default.
• W1965158002 hasConcept C62520636 @default.
• W1965158002 hasConcept C8010536 @default.
• W1965158002 hasConceptScore W1965158002C115624301 @default.
• W1965158002 hasConceptScore W1965158002C120665830 @default.
• W1965158002 hasConceptScore W1965158002C121089165 @default.
• W1965158002 hasConceptScore W1965158002C121332964 @default.
• W1965158002 hasConceptScore W1965158002C121854251 @default.
• W1965158002 hasConceptScore W1965158002C159985019 @default.
• W1965158002 hasConceptScore W1965158002C185592680 @default.
• W1965158002 hasConceptScore W1965158002C192562407 @default.
• W1965158002 hasConceptScore W1965158002C194232370 @default.
• W1965158002 hasConceptScore W1965158002C198819137 @default.
• W1965158002 hasConceptScore W1965158002C199289684 @default.
• W1965158002 hasConceptScore W1965158002C2777554867 @default.
• W1965158002 hasConceptScore W1965158002C2778189432 @default.
• W1965158002 hasConceptScore W1965158002C2778998827 @default.
• W1965158002 hasConceptScore W1965158002C2780364934 @default.
• W1965158002 hasConceptScore W1965158002C2781137303 @default.
• W1965158002 hasConceptScore W1965158002C41279357 @default.
• W1965158002 hasConceptScore W1965158002C43486711 @default.

• next