Large S isotope and trace element fractionations in pyrite of uranium roll front systems result from internally-driven biogeochemical cycle-Reference-Cited by-同舟云学术

Large S isotope and trace element fractionations in pyrite of uranium roll front systems result from internally-driven biogeochemical cycle

Published:2020-08 Issue: Volume:282 Page:113-132
ISSN:0016-7037
Container-title:Geochimica et Cosmochimica Acta
language:en
Short-container-title:Geochimica et Cosmochimica Acta

Author:

Bonnetti Christophe,Zhou Lingli,Riegler Thomas,Brugger Joël^ORCID,Fairclough Martin

Funder

National Natural Science Foundation of China

Publisher

Elsevier BV

Subject

Geochemistry and Petrology

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