Dunite channels as viable pathways for mare basalt transport in the deep lunar mantle

Author:

Beck Alyssa R.1,Morgan Zachary T.1,Liang Yan1,Hess Paul C.1

Affiliation:

1. Department of Geological Sciences; Brown University; Providence Rhode Island USA

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Geophysics

Reference18 articles.

1. Channeling instability of upwelling melt in the mantle;Aharonov;J. Geophys. Res.,1995

2. Steady-state mantle-melt interactions in one dimension: I. Equilibrium transport and melt focusing;Asimow;J. Petrol.,1999

3. The transition from porous to channelized flow due to melt-rock reaction during melt migration;Daines;Geophys. Res. Lett.,1994

4. Chemistry and liquidus phase relations of Apollo 15 red glass: Implications for the deep lunar interior;Delano;Proc. Lunar Planet. Sci. Conf. 11th,1980

5. Origin of lunar ultramafic green glasses: Constraints from phase equilibrium studies;Elkins;Geochim. Cosmochim. Acta,2000

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