Solute partitioning under continuous cooling conditions as a cooling rate indicator.

P. I.K. Onorato; R. W. Hopper; H. Yinnon; D. R. Uhlmann; L. A. Taylor; J. R. Garrison; R. Hunter

doi:10.1029/JB086iB10p09511

Solute partitioning under continuous cooling conditions as a cooling rate indicator.

P. I.K. Onorato
, R. W. Hopper
, H. Yinnon
, D. R. Uhlmann
, L. A. Taylor
, J. R. Garrison
, R. Hunter

Research output: Contribution to journal › Article › peer-review

18 Scopus citations

Abstract

A mathematical model is given for the concentration profile as a function of time, including a T-dependent partitioning of the solute between the two phases. It is illustrated by the partitioning of zirconia between ilmenite and ulvospinel. The cooling rates of a suite of Apollo 15 Elbow Crater gabbros are calculated and the implications are discussed. -K.A.R.

Original language	English (US)
Pages (from-to)	9511-9518
Number of pages	8
Journal	Journal of geophysical research
Volume	86
Issue number	B10
DOIs	https://doi.org/10.1029/JB086iB10p09511
State	Published - 1981
Externally published	Yes

ASJC Scopus subject areas

Geophysics
Forestry
Oceanography
Aquatic Science
Ecology
Water Science and Technology
Soil Science
Geochemistry and Petrology
Earth-Surface Processes
Atmospheric Science
Earth and Planetary Sciences (miscellaneous)
Space and Planetary Science
Palaeontology

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10.1029/JB086iB10p09511

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abstract = "A mathematical model is given for the concentration profile as a function of time, including a T-dependent partitioning of the solute between the two phases. It is illustrated by the partitioning of zirconia between ilmenite and ulvospinel. The cooling rates of a suite of Apollo 15 Elbow Crater gabbros are calculated and the implications are discussed. -K.A.R.",

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AU - Onorato, P. I.K.

AU - Hopper, R. W.

AU - Yinnon, H.

AU - Uhlmann, D. R.

AU - Taylor, L. A.

AU - Garrison, J. R.

AU - Hunter, R.

PY - 1981

Y1 - 1981

N2 - A mathematical model is given for the concentration profile as a function of time, including a T-dependent partitioning of the solute between the two phases. It is illustrated by the partitioning of zirconia between ilmenite and ulvospinel. The cooling rates of a suite of Apollo 15 Elbow Crater gabbros are calculated and the implications are discussed. -K.A.R.

AB - A mathematical model is given for the concentration profile as a function of time, including a T-dependent partitioning of the solute between the two phases. It is illustrated by the partitioning of zirconia between ilmenite and ulvospinel. The cooling rates of a suite of Apollo 15 Elbow Crater gabbros are calculated and the implications are discussed. -K.A.R.

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UR - https://www.scopus.com/pages/publications/0019711171#tab=citedBy

U2 - 10.1029/JB086iB10p09511

DO - 10.1029/JB086iB10p09511

M3 - Article

AN - SCOPUS:0019711171

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EP - 9518

JO - Journal of geophysical research

JF - Journal of geophysical research

IS - B10

ER -

Solute partitioning under continuous cooling conditions as a cooling rate indicator.

Abstract

ASJC Scopus subject areas

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