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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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