Tungsten Nuclear Anomalies in Planetesimal Cores
Author(s) -
Liping Qin,
Nicolas Dauphas,
M. Wadhwa,
A. Markowski,
R. Gallino,
P. E. Janney,
Claudia Bouman
Publication year - 2008
Publication title -
the astrophysical journal
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.376
H-Index - 489
eISSN - 1538-4357
pISSN - 0004-637X
DOI - 10.1086/524882
Subject(s) - planetesimal , physics , formation and evolution of the solar system , meteorite , nucleosynthesis , protoplanet , astrobiology , astrophysics , solar system , nebula , planet , astronomy , silicate , tungsten , protoplanetary nebula , planetary nebula , chondrule , chondrite , protoplanetary disk , stars , chemistry , organic chemistry
Use of the extinct 182 Hf- 182 W chronometer to constrain the timing of planetary accretion and differentiation rests ontheassumptionthatthesolarnebulahadhomogeneoustungstenisotopiccomposition.Here,wereportdeficiencies of 0.1 part in 10,000 in the abundance of 184 Win group IVB iron meteorites relative to the silicate Earth. These are mostlikelyduetoincompletemixingattheplanetesimalscale(2Y4kmradiusbodies)oftheproductsof slow(s-)and rapid (r-) neutron-capture nucleosynthesis in the solar nebula. The correction that must be applied to the 182 Hf- 182 W model age of core formation in IVB irons due to the presence of these nuclear anomalies is 0.5 Myr. Subject headingg minor planets, asteroids — nuclear reactions, nucleosynthesis, abundances — solar system: formation — stars: abundances
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