On the Isotopic Chemistry of Carbon at the Martian Surface [and Discussion]

A brief overview is presented concerning the possibilities of using meteorites, that are thought to have a Martian origin, to learn something about Mars itself. The main reasons for believing the samples are of Martian descent are also given. As an example of the sorts of information that can be obt...

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Veröffentlicht in:Philosophical transactions of the Royal Society of London. Series A: Mathematical, physical, and engineering sciences physical, and engineering sciences, 1994-11, Vol.349 (1690), p.309-321
Hauptverfasser: Wright, I. P., Pillinger, C. T., Tozer, D. C., Grady, M. M., Wallis, M. K., Hutchison, R.
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container_end_page 321
container_issue 1690
container_start_page 309
container_title Philosophical transactions of the Royal Society of London. Series A: Mathematical, physical, and engineering sciences
container_volume 349
creator Wright, I. P.
Pillinger, C. T.
Tozer, D. C.
Grady, M. M.
Wallis, M. K.
Hutchison, R.
description A brief overview is presented concerning the possibilities of using meteorites, that are thought to have a Martian origin, to learn something about Mars itself. The main reasons for believing the samples are of Martian descent are also given. As an example of the sorts of information that can be obtained by analysing Martian meteorites, previously unpublished results from a study of the carbon in shock-produced glass from one particular sample are discussed. The experimental data are used to give an insight into the potential of using isotopic data to comprehend the carbon cycle on Mars.
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ispartof Philosophical transactions of the Royal Society of London. Series A: Mathematical, physical, and engineering sciences, 1994-11, Vol.349 (1690), p.309-321
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source JSTOR Mathematics & Statistics; JSTOR Archive Collection A-Z Listing
subjects Antarctic regions
Atmospherics
Carbon dioxide
Carbonates
Cosmochemistry
Mars
Meteorites
Nakhlites
Nuclear chemistry
SNC meteorites
title On the Isotopic Chemistry of Carbon at the Martian Surface [and Discussion]
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