OXYGEN ISOTOPES IN CALCIUM-ALUMINUM-RICH INCLUSIONS FROM ENSTATITE CHONDRITES: NEW EVIDENCE FOR A SINGLE CAI SOURCE IN THE SOLAR NEBULA
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dc.contributor.author | Guan Y. | |
dc.contributor.author | McKeegan K.D. | |
dc.contributor.author | MacPherson G.J. | |
dc.date.accessioned | 2021-01-24T05:12:19Z | |
dc.date.available | 2021-01-24T05:12:19Z | |
dc.date.issued | 2000 | |
dc.identifier | https://www.elibrary.ru/item.asp?id=370226 | |
dc.identifier.citation | Earth and Planetary Science Letters, 2000, 181, 3, 271-277 | |
dc.identifier.issn | 0012-821X | |
dc.identifier.uri | https://repository.geologyscience.ru/handle/123456789/23655 | |
dc.description.abstract | Calcium-aluminum-rich inclusions (CAIs) from enstatite chondrites have large 16O excesses, similar to CAIs in carbonaceous and ordinary chondrites, and are also similar in morphology, mineralogy and Al-Mg isotopic systematics. These similarities provide new evidence that most CAIs might have formed in a single, restricted nebular locale and were then distributed unevenly throughout the various chondrite accretion regions. | |
dc.subject | OXYGEN | |
dc.subject | ISOTOPES | |
dc.subject | ENSTATITE CHONDRITES | |
dc.subject | CALCIUM-ALUMINUM INCLUSIONS | |
dc.subject | SOLAR SYSTEM | |
dc.title | OXYGEN ISOTOPES IN CALCIUM-ALUMINUM-RICH INCLUSIONS FROM ENSTATITE CHONDRITES: NEW EVIDENCE FOR A SINGLE CAI SOURCE IN THE SOLAR NEBULA | |
dc.type | Статья |
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