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The Geochemistry of some Keweenawán Metabasites from Mamainse Point, Ontario
1980The Mamainse Point Formation formed on the margin of the Late Proterozoic Keweenawan Rift. It consists of olivine- and feldspar-phyric flood basalts with felsites and conglomeratic sediments, and spans the palaeomagnetic reversal normally regarded as the boundary between Lower and Middle Keweenawan.
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Metamorphic Petrology of the Northern Tokoro Metabasites, Eastern Hokkaido, Japan
Journal of Petrology, 1991openaire +1 more source

