Abstract
Mathematical relationships between unit-cell parameters and chemical composition were developed for selected mineral phases observed with the CheMin X-ray diffractometer onboard the Curiosity rover in Gale crater. This study presents algorithms for estimating the chemical composition of phases based solely on X-ray diffraction data. The mineral systems include plagioclase, alkali feldspar, Mg-Fe-Ca C2/c clinopyroxene, Mg-Fe-Ca P21/c clinopyroxene, Mg-Fe-Ca orthopyroxene, Mg-Fe olivine, magnetite, and other selected spinel oxides, and alunite-jarosite. These methods assume compositions of Na-Ca for plagioclase, K-Na for alkali feldspar, Mg-Fe-Ca for pyroxene, and Mg-Fe for olivine; however, some other minor elements may occur and their impact on measured unit-cell parameters is discussed. These crystal-chemical algorithms can be applied to material of any origin, whether that origin is Earth, Mars, an extraterrestrial body, or a laboratory.
Original language | English (US) |
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Pages (from-to) | 848-856 |
Number of pages | 9 |
Journal | American Mineralogist |
Volume | 103 |
Issue number | 6 |
DOIs | |
State | Published - Jun 26 2018 |
Keywords
- CheMin
- Gale crater
- Mars
- Mars Science Laboratory
- Martian Rocks and Minerals
- Meteorites
- Orbiters
- Perspectives from Rovers
- X-ray diffraction
- alunite
- crystal chemistry
- jarosite
- magnetite
- olivine
- plagioclase
- pyroxene
- spinel
- unit-cell parameters
ASJC Scopus subject areas
- Geophysics
- Geochemistry and Petrology