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- W1815677470 abstract "Diamondites are fragments of polycrystalline diamond and intergrowths of silicates (mostly garnet±cpx; however they do not contain olivine). Open cavities lined with euhedral imply the presence of fluids during crystallisation. It can be demonstrated that silicates and very likely grew synchronously from the same fluid (1, 2). It has been suggested that these polycrystalline diamonds should be regarded as rocks, termed diamondites (1, 2); this nomenclature has been followed herein.Organic-like'carbon and ..." @default.
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- W1815677470 date "2010-05-01" @default.
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- W1815677470 title "'Organic-looking’ carbon and nitrogen isotope compositions in mantle derived diamondites: mantle fractionation vs. re-worked crustal organics?" @default.
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