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Another Look at Actinide Chemistry in Ca-Al-Rich Inclusions

机译:钙富铝夹杂物中Act系化学的另一种观察

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摘要

Th/U values for Allende inclusions are often high relative to the accepted solar systemudaverage (3.8). In order to understand this fractionation, we are using fission track radiographyudto measure Th and U distributions in a group of Allende inclusions. We previously reportedud(Murrell and Burnett, 1984) on TS-23, a type Bl inclusion. Th and U were found to be enriched greater than 100 x’s Cl with Th/U = 3. 8 ± 0.l in the spinel + perovskite portionudof the rim on this inclusion. The Ti-Al-rich clinopyroxene band in this rim is also enrichedudin Th and U but with Th/U = 1. In the interior of TS-23, fassaite and melilite were foundudto contain 40 ppb and 90 ppb U, respectively, with little Th-U fractionation. Also, enrichmentsudof Th and U to about 80 x's Cl were observed along grain boundaries which containedudalteration products.
机译:相对于公认的太阳系平均值(3.8),阿连德夹杂物的Th / U值通常较高。为了理解这种分级,我们使用裂变径迹摄影 ud测量一组阿连德包裹体中的Th和U分布。我们先前曾在TS-23(B1型夹杂物)上报道过 ud(Murrell和Burnett,1984)。发现Th和U富集大于100 x's Cl,Th / U =3。在该夹杂物的边缘的尖晶石+钙钛矿部分 ud中有8±0.l。在该边缘中富含Ti-Al的斜辉石带也富集了 udin Th和U,但Th / U =1。在TS-23内部,发现了玄武岩和陨石 ud包含40 ppb和90 ppb U,分别具有少量Th-U分馏。另外,沿着含有脱核产物的晶界观察到Th和U富集到约80x's Cl。

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