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- W1991344196 abstract "The Alpine peridotite massif of Lanzo (Italy) contains three generations of basic dikes (gabbros and basalts). The older gabbros are plagioclase-rich mantle segregates while the younger gabbro dikes are cumulates very similar in chemical composition to recent oceanic gabbros and gabbros from ophiolitic complexes. They both were derived from the N-type mid-ocean ridge basalt (MORB) magmas which were progressively more depleted in incompatible elements and were probably generated during a dynamic melting of a rising mantle diapir. The basaltic dikes are the N-type MORB and closely resemble the Alpine-Apennine ophiolitic basalts. They were derived from a different upper mantle source than the parental magmas of the gabbros. The source of the basalts was less depleted in light REE. The presence of basic magmas with N-type MORB affinities in the Lanzo massif is consistent with the close genetic relationship between the Alpine peridotite body and the ophiolites of the Liguro-Piemontese basin." @default.
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- W1991344196 date "1986-08-01" @default.
- W1991344196 modified "2023-09-27" @default.
- W1991344196 title "Geochemistry of basic dikes in the Lanzo massif (Western Alps): Petrogenetic and geodynamic implications" @default.
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- W1991344196 doi "https://doi.org/10.1016/0040-1951(86)90309-4" @default.
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