147SM-143ND AND 87RB-87SR AGES OF THE EUCRITE PIPLIA KALAN - A PRELIMINARY STUDY
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dc.contributor.author | Kumar A. | |
dc.contributor.author | Gopalan K. | |
dc.contributor.author | Bhandari N. | |
dc.date.accessioned | 2021-01-09T06:26:47Z | |
dc.date.available | 2021-01-09T06:26:47Z | |
dc.date.issued | 1999 | |
dc.identifier | https://elibrary.ru/item.asp?id=196860 | |
dc.identifier.citation | Geochimica et Cosmochimica Acta, 1999, , 23, 3997-4001 | |
dc.identifier.issn | 0016-7037 | |
dc.identifier.uri | https://repository.geologyscience.ru/handle/123456789/22549 | |
dc.description.abstract | Prompted by the finding that the eucrite Piplia Kalan could have retained Pu fission Xe earlier than the eucrites so far studied and hence be very ancient, we have measured a precise internal 147Sm-143Nd isochron for this meteorite. The age and initial Nd ratio relative to CHUR are 4.570 +/- 0.023 Ga and -1.3 +/- 0.7 εu, respectively. A Rb-Sr whole rock (clast) isochron for this meteorite corresponds to an age of 3.963 +/- 0.119 Ga and initial 87Sr/86Sr ratio of 0.69902 +/- 3. But initial 87Sr/86Sr ratio calculated for an age of 4.57 Ga is 0.698956 +/- 25, which is indistinguishable from 0.698970 +/- 15 reported for the angrites LEW and ADOR dated at 4.5578 +/- 0.0005 Ga. These results indicating that Piplia Kalan could have formed within only a few million years of the earliest condensates in the Solar System are strongly supported by the recent discovery of live 26Al in it. | |
dc.title | 147SM-143ND AND 87RB-87SR AGES OF THE EUCRITE PIPLIA KALAN - A PRELIMINARY STUDY | |
dc.type | Статья |
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