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Journal article

Silicon isotopes in meteorites and planetary core formation

Abstract:: The silicon (Si) isotope compositions of 42 meteorite and terrestrial samples have been determined using MC-ICPMS with the aim of resolving the current debate over their compositions and the implications for core formation. No systematic δ30Si differences are resolved between chondrites (δ30Si=-0.49±0.15‰, 2σSD) and achondrites (δ30Si=-0.47±0.11‰, 2σSD), although enstatite chondrites are consistently lighter (δ30Si=-0.63±0.07‰, 2σSD) in comparison to other meteorite groups. The data reported ...
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Publication status:: Published

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APA Style

Armytage, R., Georg, R., Savage, P., Williams, H., & Halliday, A. (2011). Silicon isotopes in meteorites and planetary core formation. GEOCHIMICA ET COSMOCHIMICA ACTA, 75(13), 3662–3676.

MLA Style

Armytage, R., et al. “Silicon Isotopes in Meteorites and Planetary Core Formation.” GEOCHIMICA ET COSMOCHIMICA ACTA, vol. 75, no. 13, 2011, pp. 3662–76.

Chicago Style

Armytage, R, R Georg, P Savage, H Williams, and A Halliday. 2011. “Silicon Isotopes in Meteorites and Planetary Core Formation.” GEOCHIMICA ET COSMOCHIMICA ACTA 75 (13): 3662–76.
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Publisher copy:: 10.1016/j.gca.2011.03.044

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+ Armytage, R More by this author

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+ Georg, R More by this author

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+ Savage, P More by this author

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+ Williams, H More by this author

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+ Halliday, A More by this author

Institution:

University of Oxford

Division:

MPLS

Department:

Earth Sciences

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Bibliographic Details

Journal:: GEOCHIMICA ET COSMOCHIMICA ACTA
Volume:: 75
Issue:: 13
Pages:: 3662-3676
Publication date:: 2011-07-01
DOI:: 10.1016/j.gca.2011.03.044
ISSN:: 0016-7037

Item Description

Language:: English
Pubs id:: pubs:151955
UUID:: uuid:13ed63de-8deb-482f-b29d-48cbc1758653
Local pid:: pubs:151955
Source identifiers:: 151955
Deposit date:: 2012-12-19

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Copyright date:: 2011

Licence:: Terms and Conditions of Use for Oxford University Research Archive

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