C13 and O18 compositions in some fresh-water carbonates associated with ultramafic rocks and serpentinites: western United States
- 3 April 2003
- journal article
- Published by Elsevier
- Vol. 35 (7) , 687-697
- https://doi.org/10.1016/0016-7037(71)90067-6
Abstract
No abstract availableKeywords
This publication has 7 references indexed in Scilit:
- Measurement of O18O16 ratios of total oxygen of carbonatesPublished by Elsevier ,2003
- Calcium-magnesium carbonate solid solutions from Holocene conglomerate cements and travertines in the Coast Range of CaliforniaGeochimica et Cosmochimica Acta, 1971
- Oxygen Isotope Fractionation in Divalent Metal CarbonatesThe Journal of Chemical Physics, 1969
- The effect of polymorphism and magnesium substitution on oxygen isotope fractionation between calcium carbonate and waterGeochimica et Cosmochimica Acta, 1969
- The Relationship between Fluids in Some Fresh Alpine-Type Ultramafics and Possible Modern Serpentinization, Western United StatesGSA Bulletin, 1969
- Improvements in Mass Spectrometers for the Measurement of Small Differences in Isotope Abundance RatiosReview of Scientific Instruments, 1950
- On the Isotopic Chemistry of Carbonates and a Paleotemperature ScaleThe Journal of Chemical Physics, 1950