These are the references the publisher has listed as being connected to the article. Please check the article itself for the full list of references which may differ. Not all references are currently linkable within the Digital Library.
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| Chakhmouradian, A. R., R. H. Mitchell, L. Horváth, and P. Tarassoff. 2001. Mont Saint-Hilaire "knowns": A look at some old minerals. Abstract in Rochester Mineralogical Symposium 2001; Rocks & Minerals 77:169-70. |
| Chao, G. Y., T. T. Chen, and J. Baker. 1980. Petarasite, a new hydrated sodium zirconium hydroxychlorosilicate mineral from Mont St-Hilaire, Quebec. Canadian Mineralogist 18:497-502. |
| Ghose, S., C. Wan, and G. Y. Chao. 1980. Petarasite, Na5Zr2Si6O18 (Cl, OH) 2H2O, a zeolite type zirconosilicate. Canadian Mineralogist 18:503-09. |
| Horváth, L., E. Pfenninger-Horváth, R. A. Gault, and P. Tarassoff. 1998. Mineralogy of the Saint-Amable sill, Varennes and Saint-Amable, Québec, Canada. Mineralogical Record 29:83-118. |
| Horváth, L., E. Pfenninger-Horváth, R. A. Gault, and P. Tarassoff. 1999. Die Mineralien des Saint-Amable Sill, Québec, Kanada (teil 1 und 2). Mineralien Welt 10(2): 53-64; 10 (3): 45-63 (in German). |
| Khomyakov, A. P. 1995. Mineralogy of hyperagpaitic alkaline rocks. Oxford: Clarendon Press. |
| Martin, R. F. 2002. People behind mineral names: Peter Tarassoff. Newsletter, Mineralogical Association of Canada 67:17. |
| Perrault, G., G. Y. Chao, and T. T. Chen. 1981. Additional data on petarasite from Mont St. Hilaire, Quebec. Canadian Mineralogist 19:411-13. |
| Tarassoff, P. 1998. Ellsworthite and the McDonald mine, Hybla, Ontario, Canada. Matrix 6(4): 159-63, 166-69. |
| Tarassoff, P. 1999. Building of Canada's national mineral collection. Matrix 7(4): 159-63, 166-69. |
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| Tarassoff, P., and R. A. Gault. 1994. Famous mineral localities: The Orford nickel mine, Québec, Canada. Mineralogical Record 25:327-45. |
| Tarassoff, P., L. Horváth, and E. Pfenninger-Horváth. 2006. Mineralogy of the Francon quarry, Montréal, Québec. Mineralogical Record 37:5-60. |
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