FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2967161851> ?p ?o ?g. }

• W2967161851 endingPage "115719" @default.
• W2967161851 startingPage "115719" @default.
• W2967161851 abstract "We constrain the lithospheric mantle in southwest Tibet to be cold, thick, and dense by considering seismological observations, isostasy, and gravity anomalies. First, virtual deep seismic sounding (VDSS) indicates that the thickness of the crust increases from 50 ± 4 km beneath the Himalaya to 70 ± 4 km in the Lhasa terrane. This implies a ‘residual topography’ (difference between isostatic elevation of crust and true elevation) of −2.4 ± 1.5 km. Taking into account deviations from isostasy, the lithospheric mantle must be dense enough to depress the surface by 0.9 to 4.5 km. Our joint inversion of fundamental-mode Rayleigh wave dispersion and receiver functions suggests that the vertically-polarised shear-wave speed (Vsv) is 4.6 ± 0.1 km s−1 at depths of 120 to 300 km. From the shear-wave speed profile, we estimate the geotherm, which is on average 200 °C below the 1350 °C adiabat, and suggest that the base of the lithosphere is at a depth of 290 ± 30 km. To match the negative buoyancy, the lithospheric must be denser, on average, than ‘normal’ fertile adiabatic mantle, which rules out a depleted (harzburgite) composition. The density excess can be explained solely by thermal contraction, but we cannot rule out additional density increases due to composition. Our observations are not consistent with a depleted Indian slab underthrusting Tibet in this region, which would result in a lower average density and lower temperatures." @default.
• W2967161851 created "2019-08-22" @default.
• W2967161851 creator A5005765081 @default.
• W2967161851 creator A5010507750 @default.
• W2967161851 creator A5038310368 @default.
• W2967161851 creator A5073494117 @default.
• W2967161851 date "2019-10-01" @default.
• W2967161851 modified "2023-10-01" @default.
• W2967161851 title "Seismological constraints on the density, thickness and temperature of the lithospheric mantle in southwestern Tibet" @default.
• W2967161851 cites W1849718941 @default.
• W2967161851 cites W1882461188 @default.
• W2967161851 cites W1892409575 @default.
• W2967161851 cites W1959912409 @default.
• W2967161851 cites W1974467019 @default.
• W2967161851 cites W1985152873 @default.
• W2967161851 cites W1988242308 @default.
• W2967161851 cites W1989579885 @default.
• W2967161851 cites W1993492957 @default.
• W2967161851 cites W2001820253 @default.
• W2967161851 cites W2005305925 @default.
• W2967161851 cites W2005536642 @default.
• W2967161851 cites W2015763705 @default.
• W2967161851 cites W2025603156 @default.
• W2967161851 cites W2045699793 @default.
• W2967161851 cites W2045733044 @default.
• W2967161851 cites W2047634839 @default.
• W2967161851 cites W2053987409 @default.
• W2967161851 cites W2057549738 @default.
• W2967161851 cites W2083266769 @default.
• W2967161851 cites W2084215965 @default.
• W2967161851 cites W2087071798 @default.
• W2967161851 cites W2088464272 @default.
• W2967161851 cites W2097382695 @default.
• W2967161851 cites W2103631538 @default.
• W2967161851 cites W2109410838 @default.
• W2967161851 cites W2112269902 @default.
• W2967161851 cites W2114660893 @default.
• W2967161851 cites W2116284155 @default.
• W2967161851 cites W2117128243 @default.
• W2967161851 cites W2122322725 @default.
• W2967161851 cites W2129900710 @default.
• W2967161851 cites W2135545468 @default.
• W2967161851 cites W2135640029 @default.
• W2967161851 cites W2139959267 @default.
• W2967161851 cites W2142937339 @default.
• W2967161851 cites W2146528904 @default.
• W2967161851 cites W2149073700 @default.
• W2967161851 cites W2153488338 @default.
• W2967161851 cites W2153774928 @default.
• W2967161851 cites W2167448438 @default.
• W2967161851 cites W2197670370 @default.
• W2967161851 cites W2216671209 @default.
• W2967161851 cites W2412791906 @default.
• W2967161851 cites W2415127810 @default.
• W2967161851 cites W2463435811 @default.
• W2967161851 cites W2510235246 @default.
• W2967161851 cites W2801792567 @default.
• W2967161851 cites W2808981438 @default.
• W2967161851 cites W2886566965 @default.
• W2967161851 doi "https://doi.org/10.1016/j.epsl.2019.115719" @default.
• W2967161851 hasPublicationYear "2019" @default.
• W2967161851 type Work @default.
• W2967161851 sameAs 2967161851 @default.
• W2967161851 citedByCount "7" @default.
• W2967161851 countsByYear W29671618512020 @default.
• W2967161851 countsByYear W29671618512021 @default.
• W2967161851 countsByYear W29671618512022 @default.
• W2967161851 countsByYear W29671618512023 @default.
• W2967161851 crossrefType "journal-article" @default.
• W2967161851 hasAuthorship W2967161851A5005765081 @default.
• W2967161851 hasAuthorship W2967161851A5010507750 @default.
• W2967161851 hasAuthorship W2967161851A5038310368 @default.
• W2967161851 hasAuthorship W2967161851A5073494117 @default.
• W2967161851 hasBestOaLocation W29671618512 @default.
• W2967161851 hasConcept C111368507 @default.
• W2967161851 hasConcept C111766609 @default.
• W2967161851 hasConcept C113740112 @default.
• W2967161851 hasConcept C127313418 @default.
• W2967161851 hasConcept C142047668 @default.
• W2967161851 hasConcept C150999391 @default.
• W2967161851 hasConcept C151730666 @default.
• W2967161851 hasConcept C162075064 @default.
• W2967161851 hasConcept C165205528 @default.
• W2967161851 hasConcept C16942324 @default.
• W2967161851 hasConcept C2776364302 @default.
• W2967161851 hasConcept C2776698055 @default.
• W2967161851 hasConcept C55510283 @default.
• W2967161851 hasConcept C67236022 @default.
• W2967161851 hasConcept C77928131 @default.
• W2967161851 hasConcept C8058405 @default.
• W2967161851 hasConcept C96342900 @default.
• W2967161851 hasConceptScore W2967161851C111368507 @default.
• W2967161851 hasConceptScore W2967161851C111766609 @default.
• W2967161851 hasConceptScore W2967161851C113740112 @default.
• W2967161851 hasConceptScore W2967161851C127313418 @default.
• W2967161851 hasConceptScore W2967161851C142047668 @default.
• W2967161851 hasConceptScore W2967161851C150999391 @default.
• W2967161851 hasConceptScore W2967161851C151730666 @default.

• next