I. Multi-Scale Dynamics of Mantle Plumes, and II. Compressible Thermochemical Convection and the Stability of Mantle Superplumes
Author: Tan, Eh
Year: 2006
Degree: Dissertation (Ph.D.)
Advisor: Gurnis, Michael C.
Committee Members: Ahrens, Thomas J.; Helmberger, Donald V.; Stevenson, David John; Tromp, Jeroen; Gurnis, Michael C.
Option: Geophysics
DOI: 10.7907/ZQ5F-9823
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
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