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Olivine occurs as phenocrysts with grain sizes up to 1 mm (smaller and more abundant than 12095 and 12240) Here we report rare earth element (ree) abundances in individual minerals from each of the three meteorites to determine their petrogenesis, parent magma compositions and relationships to other shergottites. Olivines have a brown staining probably due to shock
The maskelynites appear foliated in this section. Evidence from the paired meteorites lar 06319 and lar 12011. In addition, we calculate the relative volatile fugacities of the parental melts at the time of apatite formation.
Antarctic meteorite images for sample lar 12011 lab photo (s)
Antarctic meteorite images for sample lar 12011 thin section photo (s) : It does, however, look very similar to lar 06319. Evidence from the paired meteorites lar 06319 and lar 12011 For questions about the database or to report issues, please contact the meteoritical bulletin database editor
Questions about meteorite identification and where to get them classified will not be answered. (2016) postcrystallization metasomatism in shergottites
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