Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
4706227 | Geochimica et Cosmochimica Acta | 2005 | 16 Pages |
Abstract
The isotopic signature associated with Xe-P6 is also found only in the larger size separates. Concentration of Xe-HL increases with increasing grain size, but its relative abundance with respect to Xe-P3 and P6 is higher in smaller grain-size fractions. We argue that Xe-P6 is best seen as a variant of Xe-HL, and that they are both mixtures of a “normal” component akin to solar xenon and a slightly variable exotic component. We show that both current models of Xe-H formation can account for the observed variability, and propose a scenario according to which Xe-HL and P6 were implanted into separate diamond populations before incorporation of Xe-P3 and 129I.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Geochemistry and Petrology
Authors
J.D. Gilmour, A.B. Verchovsky, A.V. Fisenko, G. Holland, G. Turner,