FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W1915007470> ?p ?o ?g. }

• W1915007470 endingPage "4596" @default.
• W1915007470 startingPage "4572" @default.
• W1915007470 abstract "Abstract The Earth's long‐wavelength geoid anomalies have long been used to constrain the dynamics and viscosity structure of the mantle in an isochemical, whole mantle convection model. However, there is strong evidence that the seismically observed large low shear velocity provinces (LLSVPs) in the lower mantle underneath the Pacific and Africa are chemically distinct and likely denser than the ambient mantle. In this study, we have formulated dynamically self‐consistent 3‐D spherical mantle convection models to investigate how chemically distinct and dense piles above the core‐mantle boundary may influence the geoid. Our dynamic models with realistic mantle viscosity structure produce dominantly spherical harmonic degree‐2 convection, similar to that of the present‐day Earth. The models produce two broad geoid and topography highs over two major thermochemical piles in the lower mantle, consistent with the positive geoid anomalies over the Pacific and African LLSVPs. Our geoid analysis showed that the bottom layer with dense chemical piles contributes negatively to the total geoid, while the layer immediately above the chemical piles contributes positively to the geoid, canceling out the effect of the piles. Thus, the bottom part of the mantle, as a compensation layer, has zero net contribution to the total geoid, and the thickness of the compensation layer is ~1000 km or 2 to 3 times as thick as the chemical piles. Our results help constrain and interpret the large‐scale thermochemical structure of the mantle using surface observations of the geoid and topography, as well as seismic models of the mantle." @default.
• W1915007470 created "2016-06-24" @default.
• W1915007470 creator A5056470675 @default.
• W1915007470 creator A5083247969 @default.
• W1915007470 date "2015-06-01" @default.
• W1915007470 modified "2023-10-13" @default.
• W1915007470 title "The long-wavelength geoid from three-dimensional spherical models of thermal and thermochemical mantle convection" @default.
• W1915007470 cites W1489626378 @default.
• W1915007470 cites W1493404947 @default.
• W1915007470 cites W1494507377 @default.
• W1915007470 cites W1504442666 @default.
• W1915007470 cites W1517353685 @default.
• W1915007470 cites W1552025410 @default.
• W1915007470 cites W1568924786 @default.
• W1915007470 cites W1590683087 @default.
• W1915007470 cites W1608015442 @default.
• W1915007470 cites W1627691071 @default.
• W1915007470 cites W1678661852 @default.
• W1915007470 cites W1681073458 @default.
• W1915007470 cites W1751079347 @default.
• W1915007470 cites W1786439363 @default.
• W1915007470 cites W1830562234 @default.
• W1915007470 cites W1851181240 @default.
• W1915007470 cites W1868503297 @default.
• W1915007470 cites W1964564528 @default.
• W1915007470 cites W1965567608 @default.
• W1915007470 cites W1966022977 @default.
• W1915007470 cites W1968504991 @default.
• W1915007470 cites W1972370545 @default.
• W1915007470 cites W1974731988 @default.
• W1915007470 cites W1975324737 @default.
• W1915007470 cites W1980017352 @default.
• W1915007470 cites W1984800782 @default.
• W1915007470 cites W1994272913 @default.
• W1915007470 cites W1996837412 @default.
• W1915007470 cites W1996978803 @default.
• W1915007470 cites W1999741397 @default.
• W1915007470 cites W2008526841 @default.
• W1915007470 cites W2010422258 @default.
• W1915007470 cites W2012964935 @default.
• W1915007470 cites W2013012362 @default.
• W1915007470 cites W2014091139 @default.
• W1915007470 cites W2014808999 @default.
• W1915007470 cites W2015953722 @default.
• W1915007470 cites W2019827002 @default.
• W1915007470 cites W2020636993 @default.
• W1915007470 cites W2030437775 @default.
• W1915007470 cites W2037142153 @default.
• W1915007470 cites W2042242669 @default.
• W1915007470 cites W2045692715 @default.
• W1915007470 cites W2054399091 @default.
• W1915007470 cites W2055763953 @default.
• W1915007470 cites W2057139586 @default.
• W1915007470 cites W2066195054 @default.
• W1915007470 cites W2069302116 @default.
• W1915007470 cites W2071118545 @default.
• W1915007470 cites W2072891114 @default.
• W1915007470 cites W2075380580 @default.
• W1915007470 cites W2082596926 @default.
• W1915007470 cites W2084352787 @default.
• W1915007470 cites W2093905163 @default.
• W1915007470 cites W2095840192 @default.
• W1915007470 cites W2097914838 @default.
• W1915007470 cites W2104122269 @default.
• W1915007470 cites W2119605834 @default.
• W1915007470 cites W2122773073 @default.
• W1915007470 cites W2125886807 @default.
• W1915007470 cites W2132424229 @default.
• W1915007470 cites W2133984058 @default.
• W1915007470 cites W2144871560 @default.
• W1915007470 cites W2146304514 @default.
• W1915007470 cites W2148461297 @default.
• W1915007470 cites W2149834442 @default.
• W1915007470 cites W2153276003 @default.
• W1915007470 cites W2159161961 @default.
• W1915007470 cites W2160117780 @default.
• W1915007470 cites W2164817673 @default.
• W1915007470 cites W2168764039 @default.
• W1915007470 cites W2169985461 @default.
• W1915007470 cites W2171212919 @default.
• W1915007470 cites W2171947795 @default.
• W1915007470 cites W4236557437 @default.
• W1915007470 cites W948814422 @default.
• W1915007470 doi "https://doi.org/10.1002/2015jb012016" @default.
• W1915007470 hasPublicationYear "2015" @default.
• W1915007470 type Work @default.
• W1915007470 sameAs 1915007470 @default.
• W1915007470 citedByCount "20" @default.
• W1915007470 countsByYear W19150074702016 @default.
• W1915007470 countsByYear W19150074702018 @default.
• W1915007470 countsByYear W19150074702019 @default.
• W1915007470 countsByYear W19150074702020 @default.
• W1915007470 countsByYear W19150074702021 @default.
• W1915007470 countsByYear W19150074702023 @default.
• W1915007470 crossrefType "journal-article" @default.
• W1915007470 hasAuthorship W1915007470A5056470675 @default.
• W1915007470 hasAuthorship W1915007470A5083247969 @default.
• W1915007470 hasBestOaLocation W19150074701 @default.

• next