Magnesian megacrysts and matrix in the mesosiderite Lamont

Details Magnesian megacrysts and matrix in the mesosiderite Lamont Magnesian megacrysts and matrix in the mesosiderite Lamont

Mar 1997

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1997lpi....28..125b&link_type=abstract

Conference Paper, 28th Annual Lunar and Planetary Science Conference, p. 125.

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1

Igneous Rocks, Siderites, Iron, Silicates, Magnesium, Crystal Structure, Concentration (Composition), Minerals

Scientific paper

No evidence is found for the reduction of Fe from the Lamont silicates; the Fe/Mg ratios of the silicates therefore reflect their igneous history rather than a later mesosiderite history. The system from which the Lamont silicates formed is nevertheless more magnesian than that of most other mesosiderites, and may represent deeper insights into their evolution.

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