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mineral shaking table in Torino Italy Europe

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mineral shaking table in Torino Italy Europe

1. Introduction. Detrital geochronology is increasingly employed in paleotectonic reconstructions and landscape evolution problems. Detrital studies require a careful evaluation of the effects induced by hydraulic sorting, and by the variable propensity of different parent rocks to yield detrital grains of specific minerals when exposed to erosion (mineralfertility - Moecher and Samson, 2006).

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