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-Reference-Cited by-同舟云学术

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

Published:1978-10 Issue:2 Volume:41 Page:209-222
ISSN:0012-821X
Container-title:Earth and Planetary Science Letters
language:en
Short-container-title:Earth and Planetary Science Letters

Author:

Knauth L. Paul,Lowe Donald R.

Publisher

Elsevier BV

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

Reference26 articles.

1. Relationship between18O/16O ratios in coexisting carbonates, cherts, and diatomites;Degens;Bull. Am. Assoc. Pet. Geol.,1962

2. The oxygen isotopic chemistry of ancient cherts;Perry;Earth Planet. Sci. Lett.,1967

3. The oxygen isotope composition of 3,800 m.y. old metamorphosed chert and iron formation from Isukasia, West Greenland;Perry;J. Geol.,1978

4. Hydrogen and oxygen isotope ratios in nodular and bedded cherts;Knauth;Geochim. Cosmochim. Acta,1976

5. Oxygen isotope study of Precambrian banded iron formation, Hamersley Range, Western Australia;Becker;Geochim. Cosmochim. Acta,1976

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