Research on core and mantle dynamics based on the electrical conductivity of materials of the Earth and planetary interior
Author:
Affiliation:
1. Institute for Planetary Materials, Okayama University
Publisher
Japan Association of Mineralogical Sciences
Link
https://www.jstage.jst.go.jp/article/gkk/53/1/53_240109/_pdf
Reference84 articles.
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2. Badro, J., Fiquet, G., Guyot, F., Rueff, J.-P., Struzhkin, V.V., Vanko, G. and Monaco, G. (2003): Iron partitioning in Earth’s mantle: Toward a deep lower mantle discontinuity, Science, 300, 789-791.
3. Ballmer, M.D., Houser, C., Hernlund, J.W., Wentzcovitch, R.M. and Hirose, K. (2017): Persistence of strong silica-enriched domains in the Earth’s lower mantle, Nat. Geosci., 10, 236-240.
4. Chen, S., Guo, X., Yoshino, T., Jin, Z. and Li, P. (2018): Dehydration of phengite inferred by electrical conductivity measurements: Implication for the high conductivity anomalies relevant to the subduction zones. Geology, 46, 11-14.
5. Chu, T.K. and Chi, T.C. (1981): Properties of Selected Ferrous Alloying Elements, vol. III-1.
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