NOBLE GASES IN THE MOON AND METEORITES: RADIOGENIC COMPONENTS AND EARLY VOLATILE CHRONOLOGIES

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dc.contributor.author Swindle T.D.
dc.date.accessioned 2021-09-28T02:28:14Z
dc.date.available 2021-09-28T02:28:14Z
dc.date.issued 2002
dc.identifier https://elibrary.ru/item.asp?id=14031162
dc.identifier.citation Reviews in Mineralogy and Geochemistry, 2002, 47, , 47
dc.identifier.issn 1529-6466
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/30608
dc.description.abstract One of the reasons noble gases make such good tracers of processes occurring in rocks is their scarcity. Thus, a process that converts a small fraction of a relatively rare element into a noble gas can have a large effect on the noble gas. Radioactive decay can be such a process. In a meteorite which has formed very early in the solar system’s history and been little altered since, the effect can be even more dramatic. Furthermore, since radioactive decay proceeds at a known rate, radiogenic noble gases, those produced by decay, have been crucial in deciphering the chronology of...
dc.title NOBLE GASES IN THE MOON AND METEORITES: RADIOGENIC COMPONENTS AND EARLY VOLATILE CHRONOLOGIES
dc.type Статья


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