Named the Oak Point Granite in Penobscot Bay, coastal south-central ME. Unit was dated by Rb-Sr (whole rock) as 357+\-1 Ma and therefore Mississippian (or latest Devonian). The Oak Point is older than the Stonington Granite.
Source: GNU records (USGS DDS-6; Reston GNULEX).
Oak Point Granite in northern Penobscot Bay consists of light-reddish-gray to brick-red, medium-grained, coarsely porphyritic hornblende-biotite granite with subhedral phenocrysts of flesh-colored microcline and cream-colored oligoclase. Angular inclusions of country rock are numerous. Mississippian age is based on Rb-Sr whole-rock age of 349+/-1 Ma, recalculated from Brookins and Spooner (1970).
Source: GNU records (USGS DDS-6; Reston GNULEX).
For more information, please contact Nancy Stamm, Geologic Names Committee Secretary.
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