Variations of Redox conditions across the Cambrian-Ordovician GSSP (Green Point Formation) in western Newfoundland (Canada): implications from the Trace element, Mo-, U-, C-, S- and N-isotope signatures
The specific investigation of the redox conditions of the Green Point Formation sediments will allow modelling the paleoceanographic conditions on a global basis particularly because the investigated formation is the Cambrian?Ordovician GSSP, which adds to the value of the contributions of the study to understanding the global distribution of source rocks around that time interval.
Voir la description complète du projetKarem Azmy
Nalcor Energy
Earth science
Utilities
Memorial University of Newfoundland
Accelerate