Comparison of FT‐IR spectra of bulk and acid insoluble organic matter in chondritic meteorites: An implication for missing carbon during demineralization-Reference-Cited by-同舟云学术

Comparison of FT‐IR spectra of bulk and acid insoluble organic matter in chondritic meteorites: An implication for missing carbon during demineralization

Published:2019-05-08 Issue:7 Volume:54 Page:1632-1641
ISSN:1086-9379
Container-title:Meteoritics & Planetary Science
language:en
Short-container-title:Meteorit Planet Sci

Author:

Kebukawa Yoko¹^ORCID,Alexander Conel M. O'D.²^ORCID,Cody George D.¹

Affiliation:

1. Geophysical Laboratory Carnegie Institution of Washington 5251 Broad Branch Road Washington District of Columbia 20015 USA

2. Department of Terrestrial Magnetism Carnegie Institution of Washington 5241 Broad Branch Road Washington District of Columbia 20015 USA

Funder

W. M. Keck Foundation

NASA Astrobiology Institute

Japan Society for the Promotion of Science

Publisher

Wiley

Subject

Space and Planetary Science,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1111/maps.13302

Reference25 articles.

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

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

3. The Provenances of Asteroids, and Their Contributions to the Volatile Inventories of the Terrestrial Planets

4. Carbonate abundances and isotopic compositions in chondrites

5. Carbon, hydrogen and nitrogen isotopes in solvent-extractable organic matter from carbonaceous chondrites

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