Oxygen isotope geochemistry of cherts from the Onverwacht Group (3.4 billion years), Transvaal, South Africa, with implications for secular variations in the isotopic composition of cherts
- 28 October 1978
- journal article
- Published by Elsevier in Earth and Planetary Science Letters
- Vol. 41 (2), 209-222
- https://doi.org/10.1016/0012-821x(78)90011-0
Abstract
No abstract availableKeywords
This publication has 19 references indexed in Scilit:
- The Oxygen Isotope Composition of 3,800 M.Y. Old Metamorphosed Chert and Iron Formation from Isukasia, West GreenlandThe Journal of Geology, 1978
- Sedimentology of the Onverwacht Group (3.4 Billion Years), Transvaal, South Africa, and Its Bearing on the Characteristics and Evolution of the Early EarthThe Journal of Geology, 1977
- 18 O/ 16 O, D/H, and 13 C/ 12 C studies of the Tertiary igneous complex of Skye, ScotlandAmerican Journal of Science, 1977
- Oxygen isotope study of a Precambrian banded iron-formation, Hamersley Range, Western AustraliaGeochimica et Cosmochimica Acta, 1976
- Hydrogen and oxygen isotope ratios in nodular and bedded chertsGeochimica et Cosmochimica Acta, 1976
- Ancient age of the Middle Marker Horizon, Onverwacht Group, Swaziland Sequence, South AfricaEarth and Planetary Science Letters, 1972
- Significance of Oxygen and Carbon Isotope Variations in Early Precambrian Cherts and Carbonate Rocks of Southern AfricaGSA Bulletin, 1972
- Oxygen isotope evidence for large-scale interaction between meteoric ground waters and Tertiary Granodiorite Intrusions, Western Cascade Range, OregonJournal of Geophysical Research, 1971
- The oxygen isotope chemistry of ancient chertsEarth and Planetary Science Letters, 1967
- Relationship Between O18/O16 Ratios in Coexisting Minerals of Igneous and Metamorphic RocksGSA Bulletin, 1962