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.

Faculty Supervisor:

Karem Azmy

Student:

Jie Li

Partner:

Nalcor Energy

Discipline:

Geography / Geology / Earth science

Sector:

Mining and quarrying

University:

Program:

Accelerate

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