Maromas Granite Gneiss

Light-gray to buff, medium- to fine-grained granitic gneiss, composed of quartz and microcline with minor plagioclase and biotite. Central body is massive, but outlying strips are foliated and have accessory hornblende or garnet. Massive parts may be young anatectic intrusive rocks; foliated parts may include older felsic metavolcanic rocks belonging to unit Ochv. Pegmatite bodies are common in the vicinity.
State Connecticut
Name Maromas Granite Gneiss
Geologic age Devonian?
Lithologic constituents
Major
Metamorphic > GneissLight-gray to buff, medium- to fine-grained granitic gneiss, composed of quartz and microcline with minor plagioclase and biotite. Central body is massive, but outlying strips are foliated and have accessory hornblende or garnet. Massive parts may be young anatectic intrusive rocks; foliated parts may include older felsic metavolcanic rocks belonging to unit Ochv.
Incidental
Metamorphic > Metaigneous > Metavolcanicfoliated parts may include older felsic metavolcanic rocks belonging to unit Ochv
Igneous > Plutonic > Granitic > Leucocratic-granitic > PegmatitePegmatite bodies are common in the vicinity.
Comments Part of Eastern Uplands; Iapetus (Oceanic) Terrane - Bronson Hill Anticlinorium
References

Rodgers, John, compiler, 1985, Bedrock Geological Map of Connecticut: Connecticut Geological and Natural History Survey, Hartford, Connecticut, 2 sheets, scale 1:125,000.

NGMDB product
Counties Middlesex