Described here as greenish-gray, coarse-grained and horizontally sheeted granite. Exposed along Occoquan Run, from village of Occoquan to forks of Bull Run and at other places. Capped by crystalline schist. Age is Precambrian.
Source: GNU records (USGS DDS-6; Reston GNULEX).
Occoquan used informally on the State map. Described as light-gray, medium- to coarse-grained, muscovite-biotite monzogranite and lesser granodiorite and tonalite. In many places the rock has a strong quartz-rod lineation, and locally, two foliations. Intrudes Popes Head Formation, Lunga Reservoir Formation, Accotink Schist, and Sykesville Formation. The Occoquan has been dated recently at 479+/-9 Ma (U-Pb single-crystal zircon; J.N. Aleinikoff, written communication, 1993). Map symbol indicates a Cambrian and Ordovician age.
Source: GNU records (USGS DDS-6; Reston GNULEX).
Occoquan Granite intrudes Indian Run Formation in adjoining Annandale 7.5-min quad. Mose and Nagel (1982) determined an Rb-Sr whole-rock isochron age for Occoquan of 494+/-14 Ma. Preliminary U-Pb dating of zircon suggests that Occoquan may be Early Ordovician (J.N. Aleinikoff, 1992, oral commun.).
Source: GNU records (USGS DDS-6; Reston GNULEX).
Occoquan Granite has an age of 484/-8 Ma [Early Ordovician] based on weighted average of 236Pb/238U ion microprobe ages of ten zircons.
Source: GNU records (USGS DDS-6; Reston GNULEX).
For more information, please contact Nancy Stamm, Geologic Names Committee Secretary.
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