`Normal' Fe-Mg-Al-Cr Spinel Minerals in Chondritic Stratospheric IDPs

Physics

Scientific paper

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Scientific paper

'Normal' Fe-Mg-Al-Cr spinel minerals were studied in 15 chondritic
stratospheric IDPs. Most were likely to have formed in the interiors of
the IDPs by atmospheric entry heating but some may be condensates from
the solar nebula.

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