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Diamond exploration focuses on geochemical analysis of indicator minerals that are much more abundant than diamond itself. While exploration practices using peridotitic xenocrysts are robust and widely-used, similar methodologies are underdeveloped for eclogitic indicator minerals. Low-Cr garnets from mantle eclogites overlap compositionally with those of many lower-crustal lithologies transported by kimberlite. Misclassification of such crustal garnets may create “false positive” mantle signatures, possibly leading to a misdirection of exploration effort.

Robust new statistical approaches to the discrimination of mantle- and crust-derived low-Cr garnets using major and trace element data