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  Magmatic Ni-Cu-PGE prospectivity of the Labrador trough, Canada


   Cardiff School of Earth and Environmental Sciences

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  Prof W Maier  No more applications being accepted  Competition Funded PhD Project (European/UK Students Only)

About the Project

The Labrador trough remains one of the geologically least explored regions of Canada. The area is covered by extensive sills and flows of basaltic magma, emplaced into and onto a thick package of sulphide bearing pelitic rocks. This suggests enhanced prospectivity for magmatic Ni-Cu-PGE ore deposits. This project will be in collaboration with Northern Shield, a Canadian exploration company with projects across the area. The company has delineated several Ni-Cu-PGE mineralised areas and drilling is ongoing on priority targets, notably at Huckleberry. The aim of the project is to use the existing outcrop, drill core and soil geochemical samples in combination with new mapping and regional sampling to evaluate the petrogenesis of the mineralised magmatic rocks in the Labrador trough, and the prospectivity of the region for magmatic ore deposits. The student will also study the magmatic architecture of selected intrusive centres to constrain magma flow directions and the relative chronology of specific units within the intrusions, as this may allow to define vectors to ore.

Funding Notes

This studentship is very generously funded through NERC GW4+ Doctoral Training Partnership. It consists of full UK/EU tuition fees, as well as a Doctoral Stipend matching UK Research Council National Minimum (£14,296p.a. for 2016/17, updated each year) for 3.5 years.

Additional funding to the value £11,000 is available over the course of the programme for conference attendance, fieldwork allowance, travel allowance and other project costs. A further £4,000 is available in the form of as a training credits over the course of the programme for specialist training courses and/or opportunities.

References

Wardle R.J., James D.T., Scott D.J., Hall J, The southeastern Churchill Province: synthesis of a Paleoproterozoic transpressional orogeny. Can. J. Earth Sci. 39, 639–663 (2002)

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