Field and geochemical characterisitics of the Mesoarchean (~3075 ma) Ivisaartoq greenstone belt, southern West Greenland: Evidence for seafloor hydrothermal alteration in a supra-subduction oceanic crust.
A. Polat, P.W.U. Appel, Robert Frei, Y. Pan, Y. Dilek, J.C. Ordonez-Calderon, B. Fryer, J.A. Hollis, J.G. Raith
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