Controls on the stable isotope compositions of travertine from hyperalkaline springs in Oman: Insights from clumped isotope measurements

Carbonate formation at hyperalkaline springs is typical of serpentinization in peridotite massifs worldwide. These travertines have long been known to exhibit large variations in their carbon and oxygen isotope compositions, extending from apparent equilibrium values to highly depleted values. Howev...

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Bibliographic Details

Published in:	Geochimica et cosmochimica acta Vol. 192; pp. 1 - 28
Main Authors:	Falk, E.S., Guo, W., Paukert, A.N., Matter, J.M., Mervine, E.M., Kelemen, P.B.
Format:	Journal Article
Language:	English
Published:	Elsevier Ltd 01-11-2016
Subjects:	Alkaline springs Carbonate Clumped isotopes Kinetic isotope fractionation Travertine Carbonate Alkaline springs Kinetic isotope fractionation Travertine Clumped isotopes
Online Access:	Get full text
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