Strontium Isotopic Studies of Rock and Mineral Samples in the Shubenacadie Basin, Nova Scotia (original) (raw)

1986

Abstract

Strontium Isotopes of minerals within the Carboniferous (Mississippian) Windsor Group of Atlantic Canada are different from Mississippian seawater values, and indicate a re-homogenization of the Rb-Sr system occurred at 300 Ma, when hot fluids circulated and formed various Pb-Zn (such as Gays River), and Ba mineral deposits.

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