Carlos A S, Sonia M B de O, Alcides N S and Francisco J R. 2007. Geochemistry and genesis of the banded iron formations of the Gaue Formation, Quadrilatero Ferrifero, Minas Gerais, Brazil. Precambrican Research, 152: 170？206.
[25]
Danielson A, Moller P and Dulski P. 1992. The europium anomalies in banded iron formations and the thermal history of the oceanic crust. Chemical Geology, 97: 89？100.
[26]
Kato Y, Ohta I, Tsunematsu T, Watanabe Y, Isozaki Y, Maruyama S and Imai N. 1998. Rare earth element variations in mid- Archean banded iron formation: Implications for the chemistry of ocean and plate tectonics. Geochimica et Cosmochimica Acta, 62: 3475 ？3497.
[27]
Klein C. 1973. Changes in mineral assemblages with metamorphism of some banded iron-formations. Economic Geology, 68: 1075？1088.
[28]
Klein C. 2005. Some Precambrian banded iron-formations (BIFs) from around the world: Their age, geologic setting, mineralogy, metamorphism, geochemistry, and origin. American Mineralogist, 90: 1473？1499.
[29]
McLennan S B. 1989. Rare earth elements in sedimentary rocks: Influence of provenance and sedimentary processes. Reviews in Mineralogy and Geochemistry, 21(1): 169？200.
[30]
Peter J M. 2003. Ancient iron-formations: Their genesis and use in the exploration for stratiform base metal sulfide deposits, with examples from the Bathurst mining Camp. Lentz D R. Geochemistry of sediments and sedimentary rocks: Evolutionary considerations to mineral-deposit-forming environments. Geological Association of Canada, 4: 145？176.
[31]
Robert F and Ali P. 2007. Source heterogeneity for the major component of ~3.7 Ga banded iron formation (Isua Greenstone Belt, Western Greenland): Tracing the nature of interacting water masses in BIF formation. Earth and Planetary Science Letters, 253: 266？281
