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The central Maine coast is underlain by the accreted Avalon terrane which is composed of over 100 granitic and gabbroic plutons that range in age from Silurian to Carboniferous; this region is commonly referred to as the Coastal Maine Magmatic Province (CMMP) (Hogan and Sinha, 1989). Early tectonic models explained the magmatism in the CMMP as being a result of subduction during the accretion of Avalonia to North America during the Acadian Orogeny (Dewey & Kidd, 1974).

ORIENTATION, SPATIAL DISTRIBUTION, AND CHEMICAL COMPOSITION OF PALEOZOIC DIABASE DIKES ON SWANS ISLAND AND NEIGHBORING ISLANDS, PENOBSCOT BAY, MAINE