Abstract
The Tieschitz H3 chondrite contains 0.25% bulk carbon1 but concentrations of as much as 2–6% (ref. 2) occur in black, 10–20 µm-wide rims around chondrules that are thought to have accreted before the agglomeration of the stone2–5. These rims are extremely fine-grained and compact, the main constituent being an iron-rich olivine (Fa 60–65) as shown by a Debye–Sherrer X-ray diffractogram, in good agreement with the FeO/FeO + MgO matrix value2,6. To further our understanding of the rim composition and of the thermal history of the stone, we used the MOLE Raman laser microprobe7 to characterize the carbon constituent. We report here that it is a highly disordered graphite with a progressive ordering as shown by samples heated to temperatures between 300 and 600 °C. Tieschitz could not have been heated to more than 300–350 °C.
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Michel-Levy, M., Lautie, A. Microanalysis by Raman spectroscopy of carbon in the Tieschitz chondrite. Nature 292, 321–322 (1981). https://doi.org/10.1038/292321a0
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DOI: https://doi.org/10.1038/292321a0