Geochemistry of an ophiolitic complex fr
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C. Dupuy; J. Dostal; M. Leblanc
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Article
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1981
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Springer
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English
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The ophiolites of New Caledonia are composed of ultramafics overlain by mafic rocks, all of which were affected by low P metamorphism. The mafic rocks studied (gabbroic cumulates, and basaltic flows and dikes) from Montagne des Sources are similar to recent mid-ocean ridge rocks. They are olivine-no