Convection in an Internally-Heated Two-Layer System

Author:

LIMARE Angela1,JAUPART Claude1,FARNETANI Cinzia1,KAMINSKI Edouard1,SURDUCAN Emanoil2,NEAMTU Camelia2,SURDUCAN Vasile2

Affiliation:

1. National Institute for Research and Development of Isotopic and Molecular Technologies

2. Cluj-Napoca

Publisher

The Japanese Society for Multiphase Flow

Subject

General Medicine

Reference49 articles.

1. [1] Korenaga, J., Urey Ratio and the Structure and Evolution of Earth’s Mantle, Rev. Geophy., Vol. 46(2), (2008).

2. [2] Javoy, M., Kaminski, E., Guyot, F., Andrault, D., Sanloup, C., Moreira, M., Labrosse, S., Jambon, A., Agrinier, P., Davaille, A. and Jaupart, C., The Chemical Composition of the Earth, Enstatite Chondrite Models, Earth Planet. Sci. Lett., Vol. 293, 259-268 (2010).

3. [3] Schubert, G., Turcotte, D. and Olson, P., Mantle Convection in the Earth and Planets, Cambridge University Press (2001).

4. [4] Jaupart, C., Labrosse, S., Lucazeau, F. and Mareschal, J. C., Temperatures, Heat, and Energy in the Mantle of the Earth, In: Gerald Schubert (editor-in-chief), Treatise on Geophysics, Vol. 7, 223-270,Oxford:Elsevier, second edition (2015).

5. [5] Hofmann, A. W., Mantle Geochemistry: the Message from Oceanic Volcanism, Nature, Vol. 385, 219-229 (1997).

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