Geochemical differences between the Harşit Stream channel and terrace sediments (NE Turkey): Implications for mixed source rocks, weathering and mass transfer
Abstract:There are minor geochemical differences between Harşit Stream bed and terrace sediments, and these can be owing to the impacts of climatic differences and chemical weathering rather than source rock composition. The bed sediments have lower average SiO 2 , Al 2 O 3 , Fe 2 O 3 , K 2 O, TiO 2 and MnO concentrations than terrace sediments, but higher concentrations of MgO, CaO and Na 2 O. The rare earth element (REE) distributions, Eu/Eu*, (Gd/Yb) N , La/Th and (La/Yb) N ratios of the bed and terrace sediments in… Show more
Set email alert for when this publication receives citations?
scite is a Brooklyn-based organization that helps researchers better discover and understand research articles through Smart Citations–citations that display the context of the citation and describe whether the article provides supporting or contrasting evidence. scite is used by students and researchers from around the world and is funded in part by the National Science Foundation and the National Institute on Drug Abuse of the National Institutes of Health.