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Cosmogenic radioisotopes in the Almahata Sitta ureilite

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dc.contributor.author Carla, T
dc.contributor.author Narendra, B
dc.contributor.author Paolo, C
dc.contributor.author Alberto, R
dc.contributor.author Gianna, V
dc.contributor.author Neeharika, S
dc.contributor.author Peter, J
dc.contributor.author Muawia, H. S
dc.contributor.author Ballabh, G. M
dc.date.accessioned 2010-12-20T10:51:00Z
dc.date.available 2010-12-20T10:51:00Z
dc.date.issued 2010-11
dc.identifier.citation Meteoritics & Planetary Science, Vol. 45, No. 10-11, pp.1743–1750 en
dc.identifier.uri http://hdl.handle.net/2248/5282
dc.description Restricted Access en
dc.description.abstract Asteroid 2008 TC3 was predicted to fall in Sudan on October 7, 2008, and 2 months later, 15 meteorite fragments were recovered from the Nubian Desert. Most of these fragments were classified as polymict ureilites. In the largest ureilitic fragment #15, weighing 75 g, we have measured six gamma emitting radionuclides (46Sc, 57Co, 54Mn, 22Na, 60Co, and 26Al) by nondestructive whole rock counting using a sensitive gamma-ray spectrometer. The activities of 60Co, produced mainly by neutron capture in cobalt, and 26Al indicate that fragment #15 was located at a depth of 41 ± 14 cm inside the 1.5–2 m radius asteroid. The activity of other radionuclides is also consistent with this shielding depth within the asteroid. The 22Na/26Al activity ratio is higher than expected for the average cosmic ray flux, probably due to the unusually prolonged solar minimum before the fall. en
dc.language.iso en en
dc.publisher John Wiley & Sons en
dc.relation.uri http://onlinelibrary.wiley.com/doi/10.1111/j.1945-5100.2010.01135.x/abstract en
dc.rights © John Wiley & Sons en
dc.title Cosmogenic radioisotopes in the Almahata Sitta ureilite en
dc.type Article en


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