Published March 1979
| public
Book Section - Chapter
Oxygen Isotope Geothermometry of Diagenetically Altered Shales
- Others:
- Scholle, Peter A.
- Schluger, Paul R.
Abstract
The maximum temperature to which a shale has been heated as a result of burial can, in some instances, be estimated using oxygen isotope geothermometry. The isotopic fractionation, or difference between O^(18)/O^(16) ratios of two coexisting minerals which have reached isotopic equilibrium with one another, is temperature dependent. Hence, if two coexisting minerals, which have isotopically equilibrated with one another, can be separated from a shale, and if the variation of the equilibrium isotopic fractionation between these minerals is known, the temperature of equilibration can-be estimated.
Additional Information
© 1979 Society for Sedimentary Geology.Additional details
- Eprint ID
- 88397
- Resolver ID
- CaltechAUTHORS:20180731-145739803
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2018-07-31Created from EPrint's datestamp field
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2021-11-16Created from EPrint's last_modified field
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- Special publication (SEPM (Society for Sedimentary Geology))
- Series Volume or Issue Number
- 26