40 Ar/ 39 Ar age of material returned from asteroid 25143 Itokawa

The Hayabusa mission to asteroid 25143, Itokawa, brought back 2000 small particles, which most closely resemble material found in LL 4‐6 chondrites. We report an 40 Ar/ 39 Ar age of 1.3 ± 0.3 Ga for a sample of Itokawa consisting of three grains with a total mass of ~2 μg. This age is lower than the...

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Veröffentlicht in:Meteoritics & planetary science 2015-12, Vol.50 (12), p.2087-2098
Hauptverfasser: Park, Jisun, Turrin, Brent D., Herzog, Gregory F., Lindsay, Fara N., Delaney, Jeremy S., Swisher, Carl C., Uesugi, Masayuki, Karouji, Yuzuru, Yada, Toru, Abe, Masanao, Okada, Tatsuaki, Ishibashi, Yukihiro
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Sprache:eng
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Zusammenfassung:The Hayabusa mission to asteroid 25143, Itokawa, brought back 2000 small particles, which most closely resemble material found in LL 4‐6 chondrites. We report an 40 Ar/ 39 Ar age of 1.3 ± 0.3 Ga for a sample of Itokawa consisting of three grains with a total mass of ~2 μg. This age is lower than the >4.0 Ga ages measured for 75% of LL chondrites but close to one for Y‐790964 and its pairs. The flat 40 Ar/ 39 Ar release spectrum of the sample suggests complete degassing 1.3 Ga ago. Recent solar heating in Itokawa's current orbit does not appear likely to have reset that age. Solar or impact heating 1.3 Ga ago could have done so. If impact heating was responsible, then the 1.3 Ga age sets an upper bound on the time at which the Itokawa rubble pile was assembled and suggests that rubble pile creation was an ongoing process in the inner solar system for at least the first 3 billion years of solar system history.
ISSN:1086-9379
1945-5100
DOI:10.1111/maps.12564