Pg. D32-D36. Woodtick Gneiss. Intruded Waterbury Gneiss but not known to have intruded rocks stratigraphically above this formation. Age is Precambrian(?).
Source: US geologic names lexicon (USGS Bull. 1350, p. 838).
Woodtick Gneiss. Medium-grained, light- to medium-gray quartz diorite gneiss. Composed of calcic oligoclase to sodic andesine, quartz, biotite, microcline, muscovite, and garnet, with minor apatite, zircon, epidote, magnetite or ilmenite, rutile, and sphene. Emplaced probably in Precambrian time. No apparent relationship between emplacement of the Woodtick and formation of Waterbury dome. Largest body of Woodtick Gneiss not in center of dome. Type locality stated.
Type locality: about 1 mi southeast of Scoville Reservoir, Southington quadrangle, New Haven Co., central CT. Named from Woodtick.
Source: US geologic names lexicon (USGS Bull. 1350, p. 838).
Pg. 15, geologic time scale (inside front cover). Woodtick Gneiss. Samples from quartz diorite gneiss, in Southington quadrangle, New Haven County, Connecticut, yielded Pb-alpha ages of 740 +/-160 Ma and 510 +/-50 Ma (zircon); reconnaissance ages, zircons may be detrital. Ages published by Fritts (1962); recalculated using decay constants of Steiger and Jager, 1977 (Earth Planet. Sci. Letters, v. 36, p. 359-362).
Source: Publication.
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