Abstract
New, high-precision W isotope data on iron meteorites are presented that provide important constraints on the timing of silicate-metal segregation in planetesimals. Magmatic iron meteorites all have ε
Original language | English |
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Pages (from-to) | 530-542 |
Journal | Earth and Planetary Science Letters |
Volume | 241 |
DOIs | |
Publication status | Published - 2005 |