10 research outputs found

    Are the Taitao granites formed due to subduction of the Chile ridge?

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    The Taitao granites are distributed around the Late Miocene Taitao ophiolite (5.66 ± 0.33 Ma to 5.19 ± 0.15 Ma) exposed at the western tip of the Taitao peninsula, southern Chile, ~ 50 km southeast from the present day Chile triple junction. In thi

    Regioselectivity of Selenium-Mediated Carbonylation of Organolithium Compounds with Carbon Monoxide

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