Assabet Quartz Diorite and Straw Hollow Diorite are considered to be roughly equivalent in age to Sharpners Pond Diorite, which is Silurian (based on U-Th-Pb zircon age of 430 +/-5 m.y. by R.E. Zartman and R.S. Naylor, 1981, written commun.).
Source: GNU records (USGS DDS-6; Reston GNULEX).
Used as Assabet Quartz Diorite of Silurian age. Mapped undifferentiated from Straw Hollow Diorite. Intrudes Nashoba Formation.
Source: GNU records (USGS DDS-6; Reston GNULEX).
Assabet Quartz Diorite is mapped together with Straw Hollow Diorite on MA State bedrock geologic map by Zen and others (1983) because of their similar occurrence and general lithology, and their small size. Assabet covers an area of 23 sq km. Probably intrudes Marlboro Formation, although no contacts have been observed; intruded by aplite and pegmatite dikes which may be equivalent to granite that intrudes Sharpners Pond Diorite. [Papers presented as chapters in U.S. Geological Survey Professional Paper 1366 are intended as explanations and (or) revisions to MA State bedrock geologic map of Zen and others (1983) at scale of 1:250,000.]
Source: GNU records (USGS DDS-6; Reston GNULEX).
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