Types, abundances and distribution of kimberlite indicator minerals in alluvial sediments, Wawa–Kinniwabi Lake area, Northeastern Ontario: implications for the presence of diamond-bearing kimberlite

Author:

Morris T.F,Crabtree D,Sage R.P,Averill S.A

Publisher

Elsevier BV

Subject

Economic Geology,Geochemistry and Petrology

Reference51 articles.

1. Allen, J.R.L., 1984. Sedimentary Structures, Their Character and Physical Basis. Elsevier, New York.

2. Averill, S.A., McClenaghan, M.B., 1994. Distribution and character of kimberlite indicator minerals in glacial sediments, C14 and Diamond Lake kimberlite pipes, Kirkland Lake, Ontario. Geological Survey of Canada, Open File 2819, 46 pp.

3. Glacial history of northeastern Ontario. II: The Timiskaming–Algoma Area;Boissonneau;Can. J. Earth Sci.,1968

4. Velocity structure of the Kapuskasing uplift, northern Ontario, from seismic refraction studies;Boland;J. Geophys. Res.,1989

5. Coopersmith, H.G., 1993. Diamond mine discovery. In: Sheahan, P. and Chater, A. (Eds.), Diamonds: Exploration, sampling and Evaluation. Short Course. Notes. Prospectors and Developers Association of Canada, Toronto, pp. 73–108.

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