Strong tidal heating in an ultralow-viscosity zone at the core–mantle boundary of the Moon-Reference-Cited by-同舟云学术

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Strong tidal heating in an ultralow-viscosity zone at the core–mantle boundary of the Moon

Published:2014-07-27 Issue:8 Volume:7 Page:569-572
ISSN:1752-0894
Container-title:Nature Geoscience
language:en
Short-container-title:Nature Geosci

Author:

Harada Yuji,Goossens Sander,Matsumoto Koji,Yan Jianguo,Ping Jinsong,Noda Hirotomo,Haruyama Junichi

Publisher

Springer Science and Business Media LLC

Subject

General Earth and Planetary Sciences

Link

http://www.nature.com/articles/ngeo2211.pdf

Reference30 articles.

1. Ross, M. & Schubert, G. Tidal dissipation in a viscoelastic planet. J. Geophys. Res. 91, D447–D452 (1986).

2. Khan, A., Mosegaard, K., Williams, J. G. & Lognonné, P. Does the Moon possess a molten core? Probing the deep lunar interior using results from LLR and Lunar Prospector. J. Geophys. Res. 109, E09007 (2004).

3. Khan, A. & Mosegaard, K. Further constraints on the deep lunar interior. Geophys. Res. Lett. 32, L22203 (2005).

4. Efroimsky, M. Bodily tides near spin-orbit resonances. Celest. Mech. Dyn. Astron. 112, 283–330 (2012).

5. Nimmo, F., Faul, U. H. & Garnero, E. J. Dissipation at tidal and seismic frequencies in a melt-free Moon. J. Geophys. Res. 117, E09005 (2012).

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