Osmium isotope stratigraphy of a marine ferromanganese crust

Ferromanganese crusts provide records of long term change in ocean circulation and continental weathering. However, calibrating their age prior to 10 Ma has been entirely based on empirical growth rate models using Co concentrations, which have inherently large uncertainties and fail to detect hiatu...

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Xehetasun bibliografikoak
Egile Nagusiak: Klemm, V, Levasseur, S, Frank, M, Hein, JR, Halliday, A
Formatua: Journal article
Hizkuntza:English
Argitaratua: 2005