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The North America mid-Cretaceous kimberlite corridor: wet, edge-driven decompression melting of an OIB-type deep mantle source; Kjarsgaard, B A; Heaman, L M; Sarkar, C; Pearson, D G. Geochemistry, Geophysics, Geosystems (G3) vol. 18, issue 7, 2017 p. 2727-2747, https://doi.org/10.1002/2016GC006761 (NRCan Cont.# 20170071)

 

 
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