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- W2183658948 abstract "Sm-Nd and Rb-Sr isotopic data are presented for two magmatic components of the Karmoy Ophiolite Complex, SW Norway. The 493 Ma old Visnes High Leve! Complex has initial �Nd = +6.6, suggesting a primitive island are setting. The slightly older East Karmoy Layered Series has initial �Nd = +4.3, indicating a more mature island are setting. Initial 87Sr/86Sr ratios indicate seawater alteration of the Visnes High Leve! Complex, particularly the upper crustal members, b)lt no detectable interaction of seawater with the East Karmoy Layered Series. Published data reveal that ophiolitic igneous rocks have typically exchanged more of their Sr with seawater than have young MOR-generated oceanic crust. The difference is ascribed to greater circulation of hydrothermal fluids in the subduction-related environments in which many ophiolites fo�ed." @default.
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- W2183658948 date "1989-01-01" @default.
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- W2183658948 title "Seawater alteration of the Karmøy Ophiolite complex, SW Norway: Nd and Sr isotopic evidence" @default.
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