MICROSCALE VARIATIONS OF δ13C AND N CONTENT WITHIN A NATURAL DIAMOND WITH MIXED-HABIT GROWTH

dc.contributor.authorZedgenizov D.A.
dc.contributor.authorHarte B.
dc.date.accessioned2022-03-24T08:31:12Z
dc.date.available2022-03-24T08:31:12Z
dc.date.issued2004
dc.description.abstractThe variations of carbon isotope composition and nitrogen content in a natural diamond with mixed octahedral and cuboid habit have been studied with the ion microprobe technique (SIMS). The systematic variations of δ13C and Nppm in continuous growth zones belonging to both octahedral and cubic sectors have been measured. In general the octahedral growth sector in comparison with the cuboid one is richer in nitrogen by 90–300 ppm and has a slightly heavier δ13C by 0.3–1.5‰. These data show that simultaneous mixed growth of cuboid and octahedral sectors in natural diamond entails little fractionation of carbon isotopes. The observed variations are most likely due to the different nature and kinetics of growth of natural cuboid and octahedral diamonds.
dc.identifierhttps://www.elibrary.ru/item.asp?id=13449012
dc.identifier.citationChemical Geology, 2004, 205, 1-2, 169-175
dc.identifier.issn0009-2541
dc.identifier.urihttps://repository.geologyscience.ru/handle/123456789/36632
dc.titleMICROSCALE VARIATIONS OF δ13C AND N CONTENT WITHIN A NATURAL DIAMOND WITH MIXED-HABIT GROWTH
dc.typeСтатья

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