Fe and O isotopes in coesite-bearing jadeite quartzite from the Western Alps record multistage fluid-rock interactions in a continental subduction zone
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DOI: 10.1016/j.gca.2021.08.006
Abstract: Abstract Fluid is a key agent for the mass transfer between the subducting slab and the mantle wedge, which greatly affects the evolution of the crust-mantle system at convergent plate boundaries. A geochemical study was… read more here.
Keywords: coesite bearing; granitic gneiss; rock; fluid ... See more keywords