Opaques in Mercury's Crust: Additional Evidence for a Low-FeO Magma Ocean

Details Opaques in Mercury's Crust: Additional Evidence for a Low-FeO Magma Ocean Opaques in Mercury's Crust: Additional Evidence for a Low-FeO Magma Ocean

Mar 2009

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2009lpi....40.2062r&link_type=abstract

40th Lunar and Planetary Science Conference, (Lunar and Planetary Science XL), held March 23-27, 2009 in The Woodlands, Texas, i

Physics

1

Scientific paper

Laboratory spectra of opaque oxides together with MESSENGER observations
of Mercury’s surface suggest Mercury’s crust is not the
lunar highlands, modified, but is a unique array of lithologies produced
by crystallization of a low-FeO magma ocean.

Affiliated with

Also associated with

No associations

Rating

Opaques in Mercury's Crust: Additional Evidence for a Low-FeO Magma Ocean does not yet have a rating. At this time, there are no reviews or comments for this scientific paper.

If you have personal experience with Opaques in Mercury's Crust: Additional Evidence for a Low-FeO Magma Ocean, we encourage you to share that experience with our LandOfFree.com community. Your opinion is very important and Opaques in Mercury's Crust: Additional Evidence for a Low-FeO Magma Ocean will most certainly appreciate the feedback.

Rate now

Comments { 0 }

Profile ID: LFWR-SCP-O-1707234