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Changes of Ge/Si, REE+Y and SmNd isotopes in alternating Fe- and Si-rich mesobands reveal source heterogeneity of the ~2.54Ga Sijiaying banded iron formation in Eastern Hebei, China

EngineeringTrace Element GeochemistryIsotope GeochemistrySmnd IsotopesIron FormationGeologySource HeterogeneityGeochemistryChemistryGeochronologyEarth ScienceMineral Geochemistry