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- W2013293742 abstract "Abstract Annobon Island in the Gulf of Guinea is composed predominantly of volcanic rocks of alkali character ranging from basanites to trachytes. The most primitive rocks, basanites, were probably formed by variable degrees of melting of a single upper-mantle source, previously enriched in incompatible trace elements. The more differentiated rocks could have been derived from basanitic magma by fractional crystallization mainly involving kaersutite, clinopyroxene and plagioclase. It seems that, overall, there are no obvious differences in alkali basalt sequences from oceanic and continental environments." @default.
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- W2013293742 date "1982-02-01" @default.
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- W2013293742 title "Geochemistry of the volcanic island of Annobon, Gulf of Guinea" @default.
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- W2013293742 doi "https://doi.org/10.1016/0009-2541(82)90022-5" @default.
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