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In highly substituted Ca-Fe-Mg pyroxenes, several substitutional schemes may be identified. Substitution schemes 2 and 4 have not yet yielded named mineral species.

Abstracts of the Lunar and Planetary Science Conference XXI: p. (March 1990) Chikami, J., Mikouchi, T., Takeda, H., & Miyamoto, M. Mineralogy and cooling history of the calcium‐aluminum‐chromium enriched ureilite, Lewis Cliff 88774. Journal of Geophysical Research: Planets, 120(6), 1141-1159.

LEW 87051, a New Angrite: Origin in a Ca-Al-enriched Eucritic Planetesimal? Lunar and Planetary Science XXXVI.; Ling, Z., & Wang, A. Spatial distributions of secondary minerals in the Martian meteorite MIL 03346, 168 determined by Raman spectroscopic imaging. Abstracts of the Lunar and Planetary Science Conference, vol.

(1998) Chondritic Meteorites: IN: Planetary Materials (Papike, J. [Ed.]), Chapter 3, 398 pages: Mineralogical Society of America: Washington, DC, USA.

(1995) Ca-Al-rich inclusions in three Antarctic CO3 chondrites, Yamato-81020 Yamato-82050 and Yamato-790992: Record of low temperature alteration.

A variety of additional substitution schemes, which require coupling of substituents, have been identified in these pyroxenes.

Often these substitutions result in a change of species designation when they are dominant.

(2005) Mineralogy and petrology of new Antarctic nakhlite MIL 03346. Constraints on the Shock and Thermal Histories of some Components from the Unique Chondrite, Allan Hills 85085, and Their Implications.

In: Planetary Materials (Papike, JJ - Ed.), Chapter 6: 1-53: Mineralogical Society of America, Washington, DC, USA.

ESTUDIO MINERALÓGICO PRELIMINAR DE LA ALTERACIÓN HIDROTERMAL DE LA ROCA DE CAJA DE LA VETA FARALLÓN NEGRO RAMA NORTE, PROVINCIA DE CATAMARCA, ARGENTINA.

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