The Oxygen Isotope Composition of 3,800 M.Y. Old Metamorphosed Chert and Iron Formation from Isukasia, West Greenland
- 1 March 1978
- journal article
- Published by University of Chicago Press in The Journal of Geology
- Vol. 86 (2) , 223-239
- https://doi.org/10.1086/649676
Abstract
No abstract availableThis publication has 21 references indexed in Scilit:
- The nature of O18/O16 and C13/C12 secular trends in sedimentary carbonate rocksGeochimica et Cosmochimica Acta, 1976
- Hydrothermal Circulation and Geochemical Flux at Mid-Ocean RidgesThe Journal of Geology, 1976
- Generation of trondhjemitic-tonalitic liquids and Archean bimodal trondhjemite-basalt suitesGeology, 1976
- Crustal Evolution and Global Tectonics: A Petrogenic ViewGSA Bulletin, 1974
- Early Archaean Age for the Isua Iron Formation, West GreenlandNature, 1973
- Earth and Mars: Evolution of Atmospheres and Surface TemperaturesScience, 1972
- Significance of Oxygen and Carbon Isotope Variations in Early Precambrian Cherts and Carbonate Rocks of Southern AfricaGSA Bulletin, 1972
- Quartz and Magnetite: Oxygen-18-Oxygen-16 Fractionation in Metamorphosed Biwabik Iron FormationScience, 1966
- Evolution of the Oceans and the Origin of Fine-Grained DolomitesNature, 1965
- Standard for Reporting Concentrations of Deuterium and Oxygen-18 in Natural WatersScience, 1961