The parental magma for some rocks from the Norite 1 subzone of the Stillwater Complex: a lunar analog study.

Physics

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Scientific paper

The interpretation of single lunar highlands igneous samples is hindered not only by their brecciation but also by a lack of similar intensive work on terrestrial plutonic rocks. Terrestrial studies of cumulate rocks are more extensive and have a well-developed stratigraphic context. In an attempt to establish how much can be learned about the parent magma from single plutonic hand samples, single samples from three successive homogeneous but contrasting layers (anorthosite, anorthositic norite, norite) in the Stillwater Complex Norite 1 subzone were subjected to detailed petrographic and major and trace element chemical analyses.

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