Complexities in pyroxene compositions derived from absorption band centers: Examples from Apollo samples, HED meteorites, synthetic pure pyroxenes, and remote sensing data
Authors:
- 8 January 2016
- journal article
- Published by Wiley in Meteoritics & Planetary Science
- Vol. 51 (2) , 207-234
Abstract
We reexamine the relationship between pyroxene composition and near‐infrared absorption bands, integrating measurements of diverse natural and synthetic samples. We test an algorithm (PLC) involving a two‐part linear continuum removal and parabolic fits to the 1 and 2 μm bands—a computationally simple approach which can easily be automated and applied to remote sensing data. Employing a suite of synthetic pure pyroxenes, the PLC technique is shown to derive similar band centers to the modified Gaussian model. PLC analyses are extended to natural pyroxene‐bearing materials, including (1) bulk lunar basalts and pyroxene separates, (2) diverse lunar soils, and (3) HED meteorites. For natural pyroxenes, the relationship between composition and absorption band center differs from that of synthetic pyroxenes. These differences arise from complexities inherent in natural materials such as exsolution, zoning, mixing, and space weathering. For these reasons, band center measurements of natural pyroxene‐bearing materials are compositionally nonunique and could represent three distinct scenarios (1) pyroxene with a narrow compositional range, (2) complexly zoned pyroxene grains, or (3) a mixture of multiple pyroxene (or nonpyroxene) components. Therefore, a universal quantitative relationship between band centers and pyroxene composition cannot be uniquely derived for natural pyroxene‐bearing materials without additional geologic context. Nevertheless, useful relative relationships between composition and band center persist in most cases. These relationships are used to interpret M3 data from the Humboldtianum Basin. Four distinct compositional units are identified (1) Mare Humboldtianum basalts, (2) distinct outer basalts, (3) low‐Ca pyroxene‐bearing materials, and (4) feldspathic materials.Keywords
Funding Information
- National Aeronautics and Space Administration (NNX12AI96G)
This publication has 45 references indexed in Scilit:
- The lunar rock and mineral characterization consortium: Deconstruction and integrated mineralogical, petrologic, and spectroscopic analyses of mare basaltsMeteoritics & Planetary Science, 2011
- Characterization of the 1.2 μm M1 pyroxene band: Extracting cooling history from near‐IR spectra of pyroxenes and pyroxene‐dominated rocksMeteoritics & Planetary Science, 2008
- Lunar Mare Soils: Space weathering and the major effects of surface‐correlated nanophase FeJournal of Geophysical Research, 2001
- Vesta, Vestoids, and the howardite, eucrite, diogenite group: Relationships and the origin of spectral differencesMeteoritics & Planetary Science, 2001
- Ages of mare basalts on the lunar nearsideJournal of Geophysical Research, 2000
- Galileo Multispectral Imaging of the North Polar and Eastern Limb Regions of the MoonScience, 1994
- Spectral properties of plagioclase and pyroxene mixtures and the interpretation of lunar soil spectraIcarus, 1987
- Basaltic vitrophyre 15597: An undifferentiated melt sampleEarth and Planetary Science Letters, 1973
- Mineralogic and Petrologic Study of Lunar Anorthosite Slide 15415,18Science, 1972
- Apollo 12 clinopyroxenes: Chemical trendsEarth and Planetary Science Letters, 1970