Description
TAM19B-7 is the largest, unmelted fine-grained micrometeorite found to date. It has carbonaceous chondritic origins, but the oxygen isotopic composition does not match any known parent bodies. Additionally, carbon-bearing matter and isotopic composition has been extensively characterized in meteorites, but this work has not been done yet for micrometeorites. Using the NanoSIMS 50 L instrument, the bulk δ13C for TAM19B-7 was found to be 3 + 8‰, and four anomalous spots were identified with δ13C values of 12.9‰, 16.8‰, 32.7‰, and -27.1‰.
Copyright Statement
Details
Title
- Exploring Carbon-bearing Matter in an Antarctic Micrometeorite
Contributors
- Froh, Victoria (Author)
- Bose, Maitrayee (Thesis director)
- Williams, Lynda (Committee member)
- School of Earth and Space Exploration (Contributor)
- School of Molecular Sciences (Contributor)
- Barrett, The Honors College (Contributor)
Date Created
The date the item was original created (prior to any relationship with the ASU Digital Repositories.)
2021-05
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