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Geochemistry of continental rift-related rocks
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The oxidized/reduced environment of continental crust is based upon the depth of origin. So, the higher the depth, the lower the fO2. Could this relation be inverted? Is is possible to have...
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Is SiO2 mobile during the metamorphic history of the amphibolites (meaning that it can be observed in products of the previous reactions)? Is this SiO2 lost to a fluid phase during retrogression?
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