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Minerals, Volume 13, Issue 1
January 2023 - 130 articles
Cover Story: Mantle mineral inclusions in other minerals of mantle origin record different stages of the deep-seated rock formation and conditions in the mantle and allow identifying the parageneses of minerals crystallized at different P-T-fO2 conditions. Diamond is a concentrator of minerals whose compositions reflect a wide range of mantle conditions. Large megacrystals of olivine, garnet, and pyroxene grains in diamondiferous xenoliths of megacrystalline peridotites and eclogites, described previously, are characterized by the developed crack system. All diamonds which were found earlier in mantle minerals were placed in their cracks. There has been no evidence of diamond ever found as inclusion in primary olivine, garnet, or pyroxene from mantle xenoliths or in kimberlitic megacrysts. View this paper
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Minerals - ISSN 2075-163X