The importance of talc and chlorite "hybrid" rocks for volatile recycling through subduction zones; evidence fromthe high-pressure subduction melange of New Caledonia
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Spandler, Carl
Hermann, Joerg
Faure, K
Mavrogenes, John
Arculus, Richard
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Springer
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The transfer of fluid and trace elements from the slab to the mantle wedge cannot be adequately explained by simple models of slab devolatilization. The eclogite-facies mélange belt of northern New Caledonia represents previously subducted oceanic crust
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Contributions to Mineralogy and Petrology
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2037-12-31
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