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Geophysical inferences of thermal‐chemical structures in the lower mantle
Author(s) -
Yuen D. A.,
Cadek O.,
Chopelas A.,
Matyska C.
Publication year - 1993
Publication title -
geophysical research letters
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.007
H-Index - 273
eISSN - 1944-8007
pISSN - 0094-8276
DOI - 10.1029/93gl00867
Subject(s) - geology , geophysics , mantle (geology) , plume , mantle plume , thermal , hotspot (geology) , core–mantle boundary , seismic tomography , panache , seismology , tectonics , lithosphere , thermodynamics , physics
Lateral variations of the temperature field in the lower mantle have been reconstructed using new results in mineral physics and seismic tomographic data. We show that, with the application of high‐pressure experimental values of thermal expansivity and of sound velocities, the slow seismic anomalies in the lower mantle under the Pacific and Africa can be converted into realistically looking plume structures with large dimensions of 0(10³ km). The outer fringes of the plumes have an excess temperature of around 400 K. In the core of the plumes are found tongue‐like structures with extremely high thermal anomalies. These values can exceed 1200 K and are too high to be explained on the basis of thermal anomalies alone. We suggest that these major plumes in the deep mantle may be driven by both thermal and chemical buoyancies or that enhanced conductive heat‐transfer may be important there.