Economic Geology; January 2005; v. 100; no. 1;
p. 43-61; DOI: 10.2113/100.1.0043
© Society of Economic Geologists
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FIG. 2. Simplified regional geologic map of the study area, showing the
occurrence of mafic and/or ultramafic intrusions with PGE mineralization
(modified after Sutcliffe and Smith, 1988). Note the circular distribution of
mafic-ultramafic intrusions. The diabase sills belong to the igneous rocks of
the Nipigon plate.
Copyright © 2008 by Society of Economic Geologists
