Mars as the parent body of the CI carbonaceous chondrites-Reference-Cited by-同舟云学术

Mars as the parent body of the CI carbonaceous chondrites

Published:1996-05-01 Issue:9 Volume:23 Page:961-964
ISSN:0094-8276
Container-title:Geophysical Research Letters
language:en
Short-container-title:Geophys. Res. Lett.

Author:

Brandenburg John E.

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Geophysics

Link

http://www.agu.org/journals/gl/v023/i009/96GL01217/96GL01217.pdf

Reference41 articles.

1. (1982) Solar system abundances of the Grevesse N. Abundances of the elements, Meteoritic and Solar Geochim;Anders;Cosmochim. Act.,1989

2. Bjoraker , G. L. Proc. 4th Int. Conf. Mars Tuscon 69 70 1989 J. E. Brandenburg The Possible Parent Body of the CI Carbonaceous Chondrites : Mars Eos 76 17

3. Some Final Conclusions and Supporting Experiments Related to the Search for Organic Compounds on the surface of Mars;Bieman;J. Geophysical Research,1979

4. The isotopic Composition of hydrogen and carbon in the carbonaceous chondrites;Boato;Gechim. Cosmochim. Acta,1954

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1. Reply to comment: "The Nakhla Martian meteorite is a cumulate igneous rock" by A. Treiman;Mineralogy and Petrology;2003-02-01

2. Glass-bearing inclusions in olivine of the Chassigny achondrite: Heterogeneous trapping at sub-igneous temperatures;Meteoritics & Planetary Science;2000-01

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