J. A. Chamberlain; Heazlewoodite and awaruite in serpentinites of the eastern townships, Quebec. The Canadian Mineralogist ; 8 (4): 519–522. doi:
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Heazlewoodite plus magnetite and awaruite plus magnetite apparently form in different zones within ultramafic bodies as by-products of serppentinization. There is apparently an antipathy between heazlewoodite and awaruite.
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