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Compositions of pyroxenes crystallized under these conditions are summarized in Fig. 2. The Shergotty liquid composition did not produce a crystallizing assemblage at 0.1 MPa resembling the ...

Magnesium-bearing pyroxenes typically occur in basic rocks and meteorites and the crystallization history can be partly deduced from crystallographic relics consequent on phase inversion.

Given their abundance, elucidating the physical properties of pyroxenes is deemed vital in the study of rocks and minerals. Monoclinic pyroxenes, specifically, are a type of calcium-rich pyroxenes.