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Hydrothermal alteration and tectonic evolution of an intermediate- to fast-spreading back-arc oceanic crust: Late Ordovician Solund-Stavfjord ophiolite, western Norway.
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- Island Arc, 2005, v. 14, n. 4, p. 517, doi. 10.1111/j.1440-1738.2005.00481.x
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- Article