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- W2000299848 abstract "Geochemical variation and different extrusion rates of the Late-Ordovician Solund-Stavfjord Ophiolite Complex (SSOC) suggest both open and closed magma chambers. Closed chambers existed off axis and within a transform fault and are indicated by dykes and pillow lavas that evolved from high-MgO basalt to ferrobasalt by fractional crystallization of olivine, plagioclase and clinopyroxene. Hybrid magmas with ferrobasaltic composition represent open magmatic systems and are characterized by frequent eruptions of sheet flows. The SSOC is interpreted as representing either a normal or a propagating ridge-transform intersection (RTI). The propagating RTI model is favoured as it explains both the high frequency of ferrobasalt and uplift of ultramafic rocks to above the sea-level which is suggested by detrital ultramafics occurring in an ophiolitic mélange." @default.
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- W2000299848 date "1989-08-01" @default.
- W2000299848 modified "2023-10-14" @default.
- W2000299848 title "Magmatic development and tectonomagmatic models for the Solund-Stavfjord Ophiolite Complex, West Norwegian Caledonides" @default.
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- W2000299848 doi "https://doi.org/10.1016/0024-4937(89)90001-7" @default.
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