Amorphous silicates as a record of solar nebular and parent body processes—A transmission electron microscope study of fine‐grained rims and matrix in three Antarctic CR chondrites

Author:

Vollmer Christian1ORCID,Pelka Mandy1,Leitner Jan2ORCID,Janssen Arne3

Affiliation:

1. Institut für Mineralogie Westfälische Wilhelms‐Universität Corrensstr. 24 48149 Münster Germany

2. Particle Chemistry Department Max Planck Institute for Chemistry Hahn‐Meitner‐Weg 1 55128 Mainz Germany

3. Materials Performance Centre The University of Manchester Oxford Road Manchester M13 9PL UK

Funder

Deutsche Forschungsgemeinschaft

National Science Foundation

National Aeronautics and Space Administration

Smithsonian Institution

Johnson Space Center

Publisher

Wiley

Subject

Space and Planetary Science,Geophysics

Reference65 articles.

1. Why is it so difficult to classify Renazzo-type (CR) carbonaceous chondrites? – Implications from TEM observations of matrices for the sequences of aqueous alteration

2. AbreuN. M.andBrearleyA. J.2008.Petrologic and chemical effects of the onset of aqueous alteration on the matrices of CR chondrites: GRA 95229 (abstract #2013). 39th Lunar and Planetary Science Conference. CD‐ROM.

3. Early solar system processes recorded in the matrices of two highly pristine CR3 carbonaceous chondrites, MET 00426 and QUE 99177

4. AbreuN. M. CloutisE. A. andHamiltonV. E.2018.Understanding the effects of Antarctic weathering on the petrologic and spectral characteristics of pristine CR carbonaceous chondrites (abstract #1297). 49th Lunar and Planetary Science Conference. CD‐ROM.

5. The origin and evolution of chondrites recorded in the elemental and isotopic compositions of their macromolecular organic matter

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