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Major and trace element whole rock geochemistry is a simple and inexpensive tool that can be applied to monitor the similarities or differences between kimberlites. Here, we present major and trace element data for archetypal carbonate-serpentine-monticellite kimberlites from the Hall Peninsula on Baffin Island, Nunavut, Canada with a focus on the CH-6 and CH-7 pipes (181 and 428 samples respectively) on Peregrine Diamonds' 100% held Chidliak project. We also analyzed 44 samples of country rock gneisses and six samples of sedimentary carbonate xenoliths. The goals of this study were to see if whole rock geochemistry could be used to distinguish completely altered kimberlite from completely altered country rock and to differentiate kimberlite units/grade domains within a pipe, especially when the kimberlite had been weathered or altered.

A tale of two pipes: using whole rock geochemistry to see through alteration and contamination at the CH-6 &amp; CH-7 kimberlites, Chidliak kimberlite province, Baffin Island, Nunavut