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We obtained likelihoods in the lower mantle for long-wavelengthmodels of bulk sound and shear wave speed, density, and boundarytopography, compatible with gravity constraints, from normalmode splitting functions and surface wave data. Taking intoaccount the large uncertainties in Earth's thermodynamic referencestate and the published range of mineral physics data, we convertedthe tomographic likelihoods into probability density functionsfor temperature, perovskite, and iron variations. Temperatureand composition can be separated, showing that chemical variationscontribute to the overall buoyancy and are dominant in the lower1000 kilometers of the mantle.
1 Department of Earth Sciences, Utrecht University, Post Office Box 80021, 3508 TA Utrecht, Netherlands. 2 Minnesota Supercomputer Institute, Department of Geophysics University of Minnesota, Minneapolis, MN 554550219, USA.
* To whom correspondence should be addressed. E-mail: jeannot{at}geo.uu.nl
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