Reflectance spectroscopy of chromium-bearing spinel with application to recent orbital data from the Moon
-
Kelsey B. Williams
, Colin R.M. Jackson
Abstract
Visible to near-infrared (V-NIR) remote sensing observations have identified spinel in various locations and lithologies on the Moon. Experimental studies have quantified the FeO content of these spinels (Jackson et al. 2014), however the chromite component is not well constrained. Here we present compositional and spectral analyses of spinel synthesized with varying chromium contents at lunar-like oxygen fugacity (fO2). Reflectance spectra of the chromium-bearing synthetic spinels (Cr# 1–29) have a narrow (~130 nm wide) absorption feature centered at ~550 nm. The 550 nm feature, attributed to octahedral Cr3+, is present over a wide range in iron content (Fe# 8–30) and its strength positively correlates with spinel chromium content [ln(reflectancemin) = –0.0295 Cr# – 0.3708]. Our results provide laboratory characterization for the V-NIR and mid-infrared (mid-IR) spectral properties of spinel synthesized at lunar-like fO2. The experimentally determined calibration constrains the Cr# of spinels in the lunar pink spinel anorthosites to low values, potentially Cr# < 1. Furthermore, the results suggest the absence of a 550 nm feature in remote spectra of the Dark Mantle Deposits at Sinus Aestuum precludes the presence of a significant chromite component. Combined, the observation of low chromium spinels across the lunar surface argues for large contributions of anorthositic materials in both plutonic and volcanic rocks on the Moon.
Acknowledgments
The authors thank Taki Hiroi for assistance with spectral measurements and Joseph Boesenberg for assistance with EMP measurements. We thank E.A. Cloutis and S. Yamamoto for their thoughtful reviews of the manuscript. Additional thanks go to Reid F. Cooper who assisted in the early stages of this project. Support for this work was provided through NLSI (NNA09DB34A) and SSERVI (NNA13AB014).
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Manuscript handled by Boriana Mihailova.
© 2016 by Walter de Gruyter Berlin/Boston
Articles in the same Issue
- Editorial
- The most-cited journal in mineralogy and petrology (and what scientists can learn from baseball)
- Fluids in the Crust
- Fluids in the crust during regional metamorphism: Forty years in the Waterville limestone
- Research Article
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- Are covalent bonds really directed?
- Dana Medal Paper
- Constraints on the early delivery and fractionation of Earth’s major volatiles from C/H, C/N, and C/S ratios
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- Octahedral chemistry of 2:1 clay minerals and hydroxyl band position in the near-infrared: Application to Mars
- Special Collection: Advances in Ultrahigh-Pressure Metamorphism
- Multi-stage barite crystallization in partially melted UHP eclogite from the Sulu belt, China
- Spinels Renaissance: The Past, Present, and Future of those Ubiquitous Minerals and Materials
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Articles in the same Issue
- Editorial
- The most-cited journal in mineralogy and petrology (and what scientists can learn from baseball)
- Fluids in the Crust
- Fluids in the crust during regional metamorphism: Forty years in the Waterville limestone
- Research Article
- Remanent magnetization, magnetic coupling, and interface ionic configurations of intergrown rhombohedral and cubic Fe-Ti oxides: A short survey
- Research Article
- Are covalent bonds really directed?
- Dana Medal Paper
- Constraints on the early delivery and fractionation of Earth’s major volatiles from C/H, C/N, and C/S ratios
- Crossroads in Earth and Planetary Materials
- Octahedral chemistry of 2:1 clay minerals and hydroxyl band position in the near-infrared: Application to Mars
- Special Collection: Advances in Ultrahigh-Pressure Metamorphism
- Multi-stage barite crystallization in partially melted UHP eclogite from the Sulu belt, China
- Spinels Renaissance: The Past, Present, and Future of those Ubiquitous Minerals and Materials
- Crystal chemistry of spinels in the system MgAl2O4-MgV2O4-Mg2VO4
- Spinels Renaissance: The Past, Present, and Future of those Ubiquitous Minerals and Materials
- Magnetite spherules in pyroclastic iron ore at El Laco, Chile
- Special Collection: Apatite: A Common Mineral, Uncommonly Versatile
- Evidence for dissolution-reprecipitation of apatite and preferential LREE mobility in carbonatite-derived late-stage hydrothermal processes
- Special Collection: Apatite: A Common Mineral, Uncommonly Versatile
- Compositional variation of apatite from rift-related alkaline igneous rocks of the Gardar Province, South Greenland
- Special Collection: Perspectives on Origins and Evolution of Crustal Magmas
- Dynamics and thermodynamics of magma mixing: Insights from a simple exploratory model
- Special Collection: From Magmas to Ore Deposits
- Geochemistry, petrologic evolution, and ore deposits of the Miocene Bodie Hills Volcanic Field, California and Nevada
- Research Article
- Recognizing sulfate and phosphate complexes chemisorbed onto nanophase weathering products on Mars using in-situ and remote observations
- Research Article
- Crystallographic orientation relationships in host–inclusion systems: New insights from large EBSD data sets
- Research Article
- In-situ infrared spectroscopic studies of hydroxyl in amphiboles at high pressure
- Research Article
- Confined water in tunnel nanopores of sepiolite: Insights from molecular simulations
- Research Article
- Equation of state of the high-pressure Fe3O4 phase and a new structural transition at 70 GPa
- Research Article
- Reflectance spectroscopy of chromium-bearing spinel with application to recent orbital data from the Moon
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- Temperature dependences of the hyperfine parameters of Fe2+ in FeTiO3 as determined by 57Fe-Mössbauer spectroscopy
- Letter
- Accurate predictions of iron redox state in silicate glasses: A multivariate approach using X-ray absorption spectroscopy
- Research Article
- New Mineral Names