View of Polymineralic hydrothermal veins in the Paleozoic Jandaq ophiolite gabbros (Central Iran); Evidence for ingression of high temperature seawater-derived fluids in to the gabbroic section of the Paleo-Tethys oceanic crust

Return to Article Details Polymineralic hydrothermal veins in the Paleozoic Jandaq ophiolite gabbros (Central Iran); Evidence for ingression of high temperature seawater-derived fluids in to the gabbroic section of the Paleo-Tethys oceanic crust Download Download PDF

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