Serial magmatism and growth of the proterozoic continental lithosphere

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The objective of my research is to better understand the timing and process of the growth of the continents, particularly during a younger part of the Precambrian era (2500-1000 million years ago). This work is achieved through a combination of geological mapping, for example in well exposed coastal areas of northern Labrador and south Greenland, followed by geochemical and microscope analysis of the rocks, careful separation of minerals and a determination of their crystallization ages.