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Lithium Isotope Analyses of Inorganic Constituents from the Murchison Meteorite

Lithium Isotope Analyses of Inorganic Constituents from the Murchison Meteorite
Lithium Isotope Analyses of Inorganic Constituents from the Murchison Meteorite
Aqueous processes were important modifiers of solid matter during the early stages of solar system history. Lithium isotopes are sensitive indicators of such solid-liquid interactions because 7Li passes preferentially into solution and 6Li remains behind in the solid phase. Lithium isotope ratios of inorganic phases in the Murchison meteorite reveal that the value for the whole rock is simply the average of individual components with widely different isotopic compositions. 7Li content increases from chondrules to phyllosilicate-rich matrices to carbonates, as would be expected from the relative duration each component has spent during aqueous alteration on the parent asteroid.
meteors, meteoroids, laboratory methods
0004-637X
588-591
Sephton, Mark A.
fecf8f55-05e9-4211-a775-74a9edeb9048
James, Rachael H.
79aa1d5c-675d-4ba3-85be-fb20798c02f4
Bland, Philip A.
25d1d858-0e67-406b-92b3-26f9cb35b7f5
Sephton, Mark A.
fecf8f55-05e9-4211-a775-74a9edeb9048
James, Rachael H.
79aa1d5c-675d-4ba3-85be-fb20798c02f4
Bland, Philip A.
25d1d858-0e67-406b-92b3-26f9cb35b7f5

Sephton, Mark A., James, Rachael H. and Bland, Philip A. (2004) Lithium Isotope Analyses of Inorganic Constituents from the Murchison Meteorite. The Astrophysical Journal, 612 (1), 588-591. (doi:10.1086/422421).

Record type: Article

Abstract

Aqueous processes were important modifiers of solid matter during the early stages of solar system history. Lithium isotopes are sensitive indicators of such solid-liquid interactions because 7Li passes preferentially into solution and 6Li remains behind in the solid phase. Lithium isotope ratios of inorganic phases in the Murchison meteorite reveal that the value for the whole rock is simply the average of individual components with widely different isotopic compositions. 7Li content increases from chondrules to phyllosilicate-rich matrices to carbonates, as would be expected from the relative duration each component has spent during aqueous alteration on the parent asteroid.

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More information

Published date: 2004
Keywords: meteors, meteoroids, laboratory methods
Organisations: Marine Geoscience

Identifiers

Local EPrints ID: 210111
URI: http://eprints.soton.ac.uk/id/eprint/210111
ISSN: 0004-637X
PURE UUID: 44ffe4c4-abe7-45b3-81bb-e56fb98ac7a7
ORCID for Rachael H. James: ORCID iD orcid.org/0000-0001-7402-2315

Catalogue record

Date deposited: 06 Feb 2012 13:45
Last modified: 15 Mar 2024 03:30

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Contributors

Author: Mark A. Sephton
Author: Philip A. Bland

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