MOLYBDENUM ISOTOPIC COMPOSITION OF INDIVIDUAL PRESOLAR SILICON CARBIDE GRAINS FROM THE MURCHISON METEORITE - ISOTOPIC COMPOSITION OF NEON, XENON, SILICON, CARBON, AND NITROGEN

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dc.contributor.author Nicolussi G.K.
dc.contributor.author Pellin M.J.
dc.contributor.author Lewis R.S.
dc.contributor.author Davis A.M.
dc.contributor.author Amari S.
dc.contributor.author Clayton R.N.
dc.date.accessioned 2020-12-29T04:11:25Z
dc.date.available 2020-12-29T04:11:25Z
dc.date.issued 1998
dc.identifier https://elibrary.ru/item.asp?id=59374
dc.identifier.citation Geochimica et Cosmochimica Acta, 1998, , 6, 1093-1104
dc.identifier.issn 0016-7037
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/21568
dc.description.abstract We report the isotopic composition of molybdenum in twenty-three presolar SiC grains from the Murchison meteorite which have been measured by resonant ionization mass spectrometry (RIMS). Relative to terrestrial abundance (and normalized to s-process-only 96Mo), the majority of the analyzed grains show strong depletions in the p-process isotopes 92Mo and 94Mo and the r-process isotope 100Mo. Sixteen of these grains have δ-values <-600% for these three isotopes. The observed isotopic patterns of Mo from mainstream SiC grains clearly reveal the signature of s-process nucleosynthesis. Three-isotope plots of all grain data (δiMo vs. δ92Mo) show strong linear correlations with characteristic slopes. This finding suggests mixing of solar-like material and pure s-process material in the parent stars. Comparison with evolutionary calculations of nucleosynthesis and mixing in red giants suggests that low-mass thermally-pulsed symptotic giant branch (TP-AGB) stars are the most likely site for the observed s-process nucleosynthesis.
dc.title MOLYBDENUM ISOTOPIC COMPOSITION OF INDIVIDUAL PRESOLAR SILICON CARBIDE GRAINS FROM THE MURCHISON METEORITE - ISOTOPIC COMPOSITION OF NEON, XENON, SILICON, CARBON, AND NITROGEN
dc.type Статья


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