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Published in 2017 at "Chemical Geology"
DOI: 10.1016/j.chemgeo.2016.08.019
Abstract: Abstract Neoproterozoic kimberlite, ultramafic lamprophyre, and carbonatite magmatic activity was widespread across the Canadian-Greenland Shield. Models to explain the preponderance of this deeply-derived CO 2 -rich magmatism between 680–540 Ma range from impingement of multiple mantle…
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Keywords:
superior craton;
isotope;
canada;
kimberlite magmas ... See more keywords