TIMING OF ALLEGHANIAN MAGMATISM REVISITED
To test if Alleghanian magmatism occurred for a protracted length of time the ages of several granites have been re-investigated using U-Pb geochronological methods. Two concordant zircon fractions for the York granite indicate a crystallization age of 321 ± 2 Ma, in agreement with a Rb-Sr whole-rock date of 322 ± 12 Ma, and confirm that this pluton is one of the oldest Alleghanian granites yet recognized. An indistinguishable age of 320 ± 2 Ma has been determined for the nearby Churchland granite, considered to be the second largest of the Alleghanian granites. The new U-Pb date, considerably older than the Rb-Sr date of 282 ± 12 Ma, indicates that the Churchland granite is also one of the oldest known bodies. U-Pb zircon and titanite dates were determined from the Winnsboro and Liberty Hill granites to test the Rb-Sr dates of c. 295 Ma for both granites. The U-Pb dates are indistinguishable for both bodies, yielding ages of 309 ± 1 Ma for the Winnsboro granite and 309 +3.8/-1.2 Ma for the Liberty Hill granite, and thus both intrusions were emplaced 15 m.y. earlier than thought. U-Pb analyses of zircon and titanite from the Siloam granite yield an upper intercept age of 304 +3.5/-2.3 Ma, in sharp contrast to the Rb-Sr date of 263 ± 3 Ma.
These new U-Pb dates establish that Alleghanian magmatism lasted for ~ 20 m.y. rather than 60 m.y. and underscores the danger of interpreting any of the Rb-Sr dates of these granites as crystallization ages. Determining if Alleghanian magmatism occurred in distinct pulses or nearly continuously awaits further high-precision U-Pb geochronological studies.