RADIATION EFFECTS IN ZIRCON

dc.contributor.authorEwing R.C.
dc.contributor.authorWang L.
dc.contributor.authorMeldrum A.
dc.contributor.authorWeber W.J.
dc.contributor.authorCorrales L.R.
dc.date.accessioned2021-12-18T07:26:47Z
dc.date.available2021-12-18T07:26:47Z
dc.date.issued2003
dc.description.abstractThe widespread distribution of zircon in the continental crust, its tendency to concentrate trace elements, particularly lanthanides and actinides, its use in age-dating, and its resistance to chemical and physical degradation have made zircon the most important accessory mineral in geologic studies. Because zircon is highly refractory, it also has important industrial applications, including its use as a lining material in high-temperature furnaces. However, during the past decade, zircon has also been proposed for advanced technology applications, such as a durable material for the immobilization of plutonium (Ewing et al. 1995) or, when modified by ion-beam irradiation, as an optic waveguide material (Babsail et al. 1991). In all of these applications, the change in properties as a function of increasing radiation dose is crucial (see for example, Lumpkin 2001). In this chapter, we summarize the state-of-knowledge on the radiation damage accumulation process in zircon.
dc.identifierhttps://www.elibrary.ru/item.asp?id=31327644
dc.identifier.citationReviews in Mineralogy and Geochemistry, 2003, 53, , 53
dc.identifier.issn1529-6466
dc.identifier.urihttps://repository.geologyscience.ru/handle/123456789/33579
dc.subjectzircon
dc.titleRADIATION EFFECTS IN ZIRCON
dc.typeСтатья

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