Transition between tholeiitic and alkali basalts: Petrographical and geochemical evidence from Fangataufa, Pacific Ocean, and Kerguelen, Indian Ocean
The transition from tholeiitic to alkali basalts, which is well established in the Hawaiian series, is exposed in numerous other oceanic islands. Two case studies are presented here, which illustrate the more general geochemical evolution with time from “subalkaline” to “alkaline” compositions: Fang...
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Veröffentlicht in: | GEOCHEMICAL JOURNAL 1994/12/20, Vol.28(6), pp.489-515 |
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