Geochemistry, Nd, Pb and Sr isotope systematics, and U-Pb zircon ages of the Neoarchean Bad Vermilion Lake greenstone belt and spatially associated granitic rocks, western Superior Province, Canada
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文摘

The Neoarchean Bad Vermilion Lake greenstone contains mafic to felsic volcanic rocks.

The belt formed in an arc setting.

The belt originated at about 2720 Ma.

The belt can be defined as an Archean subduction-related ophiolite.

Metamorphism modified Nd, Pb and Sr isotopic compositions.

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