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The crystal structure of goethite, FeO(OH), has two distinct oxygen sites, one with exclusively Fe-O bonds, the other with bonds to both iron and hydrogen. We developed a method to assess the oxygen isotope contrast between these sites by measuring b
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::a02f7a166264a73eac9a3380d524f306
https://resolver.caltech.edu/CaltechAUTHORS:20200330-070628054
https://resolver.caltech.edu/CaltechAUTHORS:20200330-070628054
