학술논문
Trace elements and isotope geochemistry (C, O, Fe, Cr) of the Cauê iron formation, Quadrilátero Ferrífero, Brazil: Evidence for widespread microbial dissimilatory iron reduction at the Archean/Paleoproterozoic transition
Document Type
Article
Author
Source
In Precambrian Research September 2017 298:39-55
Subject
Language
ISSN
0301-9268