Granulite Clasts of Intermediate Mg* in Lunar Meteorite Alha 81005: Chemical Compositions and Origins

نویسندگان

  • K. E. Rahilly
  • A. H. Treiman
چکیده

Lunar highland meteorites contain fragments of metamorphic granulites with a wide range of Mg* (molar Mg/(Mg+Fe)) [1], between that of Mg-suite plutonics and magnesian anorthositic granulites (MAG), and those of ferroan anorthosites (FAN), Figure 1 [2,3]. The intermediate-Mg* granulites have been inferred (explicitly or implicitly) to represent mixtures of FAN and MAG or Mg-suite rocks. To test this inference, we analyzed granulite clasts in lunar meteorite ALHA 81005, which include MAG, FAN composition, and those of intermediate Mg*. Most of the intermediate-Mg* granulites cannot be simple binary mixtures of MAG and one FAN composition. Thus, the intermediate-Mg* granulites probably formed from several precursor materials, and likely by several mechanisms, including solid-state diffusion.

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تاریخ انتشار 2009