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Brecciation of CI Chondrites: Uncoupled D/H and Elemental Ratios in Individual Fragments — Evidence for a Low Variability in D/H Ratio After Alteration

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Hoppe,  P.
Particle Chemistry, Max Planck Institute for Chemistry, Max Planck Society;

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Patzek, M., Hoppe, P., Alfing, J., & Bischoff, A. (2017). Brecciation of CI Chondrites: Uncoupled D/H and Elemental Ratios in Individual Fragments — Evidence for a Low Variability in D/H Ratio After Alteration. Meteoritics and Planetary Science, 52, A266-A266.


Cite as: https://hdl.handle.net/21.11116/0000-0001-56D5-E
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