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The implication of the oxygen isotope records in coexisting cherts and phosphates

Epstein, S. (1988) The implication of the oxygen isotope records in coexisting cherts and phosphates. Chemical Geology, 70 (1-2). p. 183. ISSN 0009-2541. http://resolver.caltech.edu/CaltechAUTHORS:20131112-113407433

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Abstract

The δ^(18)O values of coexisting mineral pairs and H_2O which are in isotopic equilibrium can provide absolute temperatures of equilibration and the δ^(18)O of the fluid medium provided that the relationships between the fractionation factors among the different components and temperature have been calibrated.


Item Type:Article
Related URLs:
URLURL TypeDescription
http://dx.doi.org/10.1016/0009-2541(88)90737-1DOIArticle
http://www.sciencedirect.com/science/article/pii/0009254188907371PublisherArticle
Additional Information:© 1988 Published by Elsevier B.V.
Record Number:CaltechAUTHORS:20131112-113407433
Persistent URL:http://resolver.caltech.edu/CaltechAUTHORS:20131112-113407433
Official Citation:S. Epstein, The implication of the oxygen isotope records in coexisting cherts and phosphates, Chemical Geology, Volume 70, Issues 1–2, 1 August 1988, Page 183, ISSN 0009-2541, http://dx.doi.org/10.1016/0009-2541(88)90737-1. (http://www.sciencedirect.com/science/article/pii/0009254188907371)
Usage Policy:No commercial reproduction, distribution, display or performance rights in this work are provided.
ID Code:42390
Collection:CaltechAUTHORS
Deposited By: Ruth Sustaita
Deposited On:12 Nov 2013 22:07
Last Modified:12 Nov 2013 22:07

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