Cordierite-spinel troctolite, a new magnesium-rich lithology from the lunar highlands

Computer Science

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Moon, Highlands, Troctolite, Magnesium, Lithology, Samples, Lunar, Spinel, Cordierite, Breccias, Apollo 15, 15295, Mineralogy, Origin, Composition, Formation, Metamorphism, Clasts, Crust, Depth, Abundance, Photomicrographs, Laboratory Studies, Crystallization, Cumlates

Scientific paper

A clast of spineltroctolite containing 8 percent cordierite (Mg2,Al4Si5O18) has been identified among the constituents of Apollo 15 regolith breccia 15295. The cordierite and associated anorthite, forsteritic olivine, and pleonaste spinel represent a new, Mg-rich lunar highlands lithology that formed by metamorphism of an igneous spinel cumulate. The cordierite-forsterite pair in the assemblage is stable at a maximum pressure of 2.5 kilobars, equivalent to a depth of 50 kilometers, or 10 kilometers above the lunar crust-mantle boundary. The occurrence of the clast indicates that spinel cumulates are a more important constituent of the lower lunar crust than has been recognized. The rarity of cordierite-spinel troctolite among lunar rock samples suggests that it is excavated only by large impact events, such as the one that formed the adjacent Imbrium Basin.

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