Nanoscale mineralogy and organic structure in Orgueil (CI) and EET 92042 (CR) carbonaceous chondrites studied with AFM‐IR spectroscopy-Reference-Cited by-同舟云学术

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Nanoscale mineralogy and organic structure in Orgueil (CI) and EET 92042 (CR) carbonaceous chondrites studied with AFM‐IR spectroscopy

Published:2021-12-31 Issue:1 Volume:57 Page:3-21
ISSN:1086-9379
Container-title:Meteoritics & Planetary Science
language:en
Short-container-title:Meteorit & Planetary Scien

Author:

Phan Van T. H.¹^ORCID,Rebois Rolando¹,Beck Pierre¹,Quirico Eric¹,Bonal Lydie¹,Noguchi Takaaki²^ORCID

Affiliation:

1. Institut de Planétologie et d’Astrophysique de Grenoble (IPAG) Université Grenoble Alpes/CNRS‐INSU UMR 5274 Grenoble F‐38041 France

2. Division of Earth and Planetary Sciences Graduate School of Science Kyoto University Kitashirakawaoiwake‐cho, Sakyo‐ku Kyoto 606‐8502 Japan

Publisher

Wiley

Subject

Space and Planetary Science,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1111/maps.13773

Reference52 articles.

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

2. The nature, origin and modification of insoluble organic matter in chondrites, the major source of Earth’s C and N

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

4. Deuterium enrichments in chondritic macromolecular material—Implications for the origin and evolution of organics, water and asteroids

5. Interstellar grains in meteorites: I. Isolation of SiC, graphite and diamond; size distributions of SiC and graphite

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