Controls on iron-isotope fractionation in organic-rich sediments (Kimmeridge Clay, Upper Jurassic, southern England)

This study explores the fractionation of iron isotopes (57 Fe/54Fe) in an organic-rich mudstone succession, focusing on core and outcrop material sampled from the Upper Jurassic Kimmeridge Clay Formation type locality in south Dorset, UK. The organic-rich environments recorded by the succession prov...

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Détails bibliographiques
Auteurs principaux: Matthews, A, Morgans-Bell, H, Emmanuel, S, Jenkyns, H, Erel, Y, Halicz, L
Format: Journal article
Langue:English
Publié: 2004