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- W1549389966 abstract "The dynamic interaction of mantle plumes with subducted slabs and plate-scale flow is studied in Part I. We found that plumes preferentially develop on the edge of slabs and that a substantial amount of hot mantle can be trapped beneath slabs over long periods of time, leading to mega-plume formation. We used the solver-coupling technique to study the deflection of plume conduits and compare our result with the parameterized approach. The stability of mantle superplumes in compressible thermo-chemical convection is studied in Part II. The depth-dependent chemical density profile, caused by composition-dependent compressibility, is the preferred mechanism to stabilize the superplum" @default.
- W1549389966 created "2016-06-24" @default.
- W1549389966 creator A5027013282 @default.
- W1549389966 date "2006-01-01" @default.
- W1549389966 modified "2023-09-26" @default.
- W1549389966 title "I. Multi-scale dynamics of mantle plumes and II. Compressible thermo-chemical convection and the stability of mantle superplumes" @default.
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- W1549389966 doi "https://doi.org/10.7907/zq5f-9823." @default.
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