Abstract
Initial iodine isotopic compositions for 10 individual chondrules show a total range of 6.5%, corresponding with an age difference of 1.6 m.y. Possible interpretations are distinct formation ages, metamorphic ages, or isotopic inhomogeneities in the early solar system, and constrain models for chondrule formation. Two chondrules show evidence of either isotopic inhomogeneities or disturbances of their I-Xe systems. -B.M.
Original language | English (US) |
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Pages (from-to) | A303-A317 |
Journal | Journal of geophysical research |
Volume | 87 |
Issue number | Supplement |
DOIs | |
State | Published - 1982 |
Externally published | Yes |
ASJC Scopus subject areas
- Geophysics
- Forestry
- Oceanography
- Aquatic Science
- Ecology
- Water Science and Technology
- Soil Science
- Geochemistry and Petrology
- Earth-Surface Processes
- Atmospheric Science
- Earth and Planetary Sciences (miscellaneous)
- Space and Planetary Science
- Palaeontology