Abstract
Of all the geological sources of evidence that have been quoted as to the composition of the atmosphere and surface waters in the Archaean and early Proterozoic, banded iron-formations (BIF) deserve special attention. Not only to they occur in vast quantities and widely distributed on the continents, not only are they virtually restricted to rocks older than about 2 Gyr, but they are chemical sediments that exhibit extraordinary lateral continuity in individual bands, and also sudden changes in composition from one band to another that must ultimately depend on simultaneous changes in the composition of the water from which they formed.
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References
Airey, P.L. and Dainton, F.S., 1966. The photochemistry of aqueous solutions of Fe(II). I. Photoelectron detachment from ferrous and ferrocyanide ions. Proc. R. Soc. London, A291: 340–352.
Becker, R.H. and Clayton, R.N., 1972. Carbon isotopic evidence for the origin of a banded iron-formation in Western Australia. Geochim. Cosmochim. Acta, 36: 577–595.
Broecker, W.S., 1971. A kinetic model for the chemical composition of sea water. Quatern. Res., 1: 188–207.
Cairns-Smith, A.G., 1978. Precambrian solution photochemistry, inverse segregation, and banded iron formations. Nature, 276: 807–808.
Cloud, P., 1973. Paleoecological significances of banded iron-formation. Econ. Geol., 68: 1135–1143.
Eugster, H.P. and Chou, I-Ming, 1973. The depositional environments of Precambrian banded iron-formations. Econ. Geol., 68: 1144–1168.
Frost, B.R., 1978. Some aspects of the sedimentary and diagenetic environment of Proterozoic banded iron-formations - A discussion. Econ. Geol., 73, 1369–1371.
Harder, H., 1964. Können Eisensäuerlinge die Genese der Lahn-Dill-Erze erklären? Beitr. Miner. Petrogr., 9: 379–422.
Harder, H. and Flehmig, W., 1970. Quarzsynthese bei tiefen Temperaturen. Geochim. Cosmochim. Acta, 34: 295–305.
Holland, H.D., 1973. The oceans: A possible source of iron in iron-formations. Econ. Geol., 68: 1169–1172.
Jortner, J. and Stein, G., 1962. The photochemical evolution of hydrogen from aqueous solutions of ferrous ions. J. Phys. Chem., 66: 1258–1271.
Klein, C. and Bricker, O.P., 1977. Some aspects of the sedimentary and diagenetic environment of Proterozoic banded iron-formations. Econ. Geol., 72: 1457–1470.
La Berge, G.L., 1966. Altered pyroclastic rocks in iron formation in the Hamersley Range Western Australia. Econ. Geol., 61: 147–161.
Langmuir, D., 1969. The Gibbs free energies of substances in the system Fe-02-H20–0O2 at 25°C. U.S. Geol. Surv. Prof. Paper, 650-B: 180–184.
Mel’nik, IU.P., 1973. Physiochemical Conditions of Formation of the Precambrian Ferruginous Quartzites. Kiev Akad. Nauk Ukrainskoi SSR Institut geokhimii i fiziki mineralov (Izdatel’stvo “Naukova Dumka”), 272 pp (in Russian).
Trendall, A.F., 1965. Progress report on the Brockman Iron Formation in the WittenoomYampire area. Geol. Surv. West. Aust. Ann. Rep., 1964: 55–65.
Trendall, A.F., 1972. Revolution in earth history. J. Geol. Soc. Aust., 19: 287–311.
Trendall, A.F. and Blockley, J.G., 1970. The Iron Formations of the Precambrian Hamersley Group, Western Australia. Bull. Geol. Surv. West. Aust., 119, 366 pp.
Trendall, A.F. and Pepper, R.S., 1977. Chemical Composition of the Brockman Iron Formation. Geol. Surv. West. Aust. Rec. No. 1976/25.
Wagman, D.D., Evans, W.H., Parker, V.B., Halow, I., Bailey, S.M. and Schur, R.H., 1969. Selected Values of Chemical Thermodynamic Properties. U.S. Nat. Bur. Stand. Tech. Note 270–4, 152 pp.
Zelenov, K.K., 1958. Leaching and transportation of dissolved iron by thermal waters of Ebeko volcano. Dokl. Akad. Nauk SSSR, 120: 1089–1092 (in Russian).
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© 1980 Australian Academy of Science
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Ewers, W.E. (1980). Chemical Conditions for the Precipitation of Banded Iron-Formations. In: Trudinger, P.A., Walter, M.R., Ralph, B.J. (eds) Biogeochemistry of Ancient and Modern Environments. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-48739-2_9
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DOI: https://doi.org/10.1007/978-3-642-48739-2_9
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