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- W4220886637 endingPage "117477" @default.
- W4220886637 startingPage "117477" @default.
- W4220886637 abstract "Thermal transport in subducted slabs and mantle critically influences their thermo-chemical evolution and dynamics, where the thermal conductivity controls the magnitude of conductive heat transfer. Here we investigate high-pressure thermal conductivities of stishovite and new-hexagonal-aluminous (NAL) phase, two major slab minerals in the shallow lower mantle, and their impacts on slab dynamics. Pure and Al-bearing stishovite exhibit conductivities of 60–70 and 30–40 W m−1 K−1, respectively, at 25–60 GPa and 300 K, much higher than the Fe-bearing NAL, 10–33 W m−1 K−1, and assemblage of a pyrolitic mantle or subducted basaltic crust. Numerical simulations indicate that subducted crustal materials particularly with local silica-enrichment would have efficient thermal conduction which promotes faster warming of a sinking slab, altering dynamic stability of slab materials and leading to slab stagnation and crust detachment in the shallow lower mantle. Conductive heat transfer in silica-enriched regions along subducted slabs in the shallow lower mantle can be more influential on mantle dynamics than previously thought." @default.
- W4220886637 created "2022-04-03" @default.
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- W4220886637 date "2022-04-01" @default.
- W4220886637 modified "2023-09-27" @default.
- W4220886637 title "High thermal conductivity of stishovite promotes rapid warming of a sinking slab in Earth's mantle" @default.
- W4220886637 cites W1912372454 @default.
- W4220886637 cites W1926355678 @default.
- W4220886637 cites W1932628490 @default.
- W4220886637 cites W1935223635 @default.
- W4220886637 cites W1964262193 @default.
- W4220886637 cites W1967371674 @default.
- W4220886637 cites W1968948224 @default.
- W4220886637 cites W1972147484 @default.
- W4220886637 cites W1977950400 @default.
- W4220886637 cites W1980654499 @default.
- W4220886637 cites W1980991404 @default.
- W4220886637 cites W1983679738 @default.
- W4220886637 cites W1994775909 @default.
- W4220886637 cites W1997704409 @default.
- W4220886637 cites W2000614548 @default.
- W4220886637 cites W2001580387 @default.
- W4220886637 cites W2004881801 @default.
- W4220886637 cites W2009590881 @default.
- W4220886637 cites W2014961616 @default.
- W4220886637 cites W2021065582 @default.
- W4220886637 cites W2021986866 @default.
- W4220886637 cites W2022181810 @default.
- W4220886637 cites W2025063939 @default.
- W4220886637 cites W2028901741 @default.
- W4220886637 cites W2030092125 @default.
- W4220886637 cites W2030645740 @default.
- W4220886637 cites W2031407346 @default.
- W4220886637 cites W2034570846 @default.
- W4220886637 cites W2037703649 @default.
- W4220886637 cites W2038574271 @default.
- W4220886637 cites W2040457913 @default.
- W4220886637 cites W2044434947 @default.
- W4220886637 cites W2048152700 @default.
- W4220886637 cites W2051793567 @default.
- W4220886637 cites W2052917852 @default.
- W4220886637 cites W2056855836 @default.
- W4220886637 cites W2061848266 @default.
- W4220886637 cites W2062142590 @default.
- W4220886637 cites W2065595161 @default.
- W4220886637 cites W2066263948 @default.
- W4220886637 cites W2071365268 @default.
- W4220886637 cites W2073355734 @default.
- W4220886637 cites W2073818231 @default.
- W4220886637 cites W2084544096 @default.
- W4220886637 cites W2091265660 @default.
- W4220886637 cites W2091747361 @default.
- W4220886637 cites W2095440947 @default.
- W4220886637 cites W2103507313 @default.
- W4220886637 cites W2106659890 @default.
- W4220886637 cites W2108136361 @default.
- W4220886637 cites W2108597026 @default.
- W4220886637 cites W2121437383 @default.
- W4220886637 cites W2133178214 @default.
- W4220886637 cites W2133515186 @default.
- W4220886637 cites W2189820340 @default.
- W4220886637 cites W2206529978 @default.
- W4220886637 cites W2253530107 @default.
- W4220886637 cites W2502040090 @default.
- W4220886637 cites W2559796282 @default.
- W4220886637 cites W2569663946 @default.
- W4220886637 cites W2575571876 @default.
- W4220886637 cites W2604215719 @default.
- W4220886637 cites W2606876715 @default.
- W4220886637 cites W2662079224 @default.
- W4220886637 cites W2738854209 @default.
- W4220886637 cites W2796366107 @default.
- W4220886637 cites W2946581359 @default.
- W4220886637 cites W2946751170 @default.
- W4220886637 cites W2947988340 @default.
- W4220886637 cites W2994649007 @default.
- W4220886637 cites W2999891772 @default.
- W4220886637 cites W3004565749 @default.
- W4220886637 cites W3027510264 @default.
- W4220886637 cites W3048584373 @default.
- W4220886637 cites W3120796805 @default.
- W4220886637 cites W3165010465 @default.
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- W4220886637 doi "https://doi.org/10.1016/j.epsl.2022.117477" @default.
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