U-PB SHRIMP-RG ANALYSIS OF ZIRCON IN MIGMATITIC ROCKS IN THE SOUTHEASTERN PART OF THE NASHOBA TERRANE, EASTERN MASSACHUSETTS
The Marlboro Formation and Shawsheen Gneiss in the southeastern NT are Cambrian-Ordovician mafic metavolcanic, and metasedimentary rocks. They are locally migmatitic and preserve northwest-side-down and northwest-side-up asymmetric folds and S-C fabrics. Two samples from the Marlboro Formation in the south and Shawsheen Gneiss in the north, and one sample from an undeformed crosscutting dike in the Marlboro Formation were collected for U-Pb zircon SHRIMP-RG analysis. In the two migmatitic samples, zircon cathodoluminescence (CL) images display cores with oscillatory and sector zonations, overgrown by CL-dark mantles and CL-bright rims. Cores and mantles are separated by CL-bright dissolution margins. Mantles and rims are concordant in CL and have the same ages, and may reflect continuous growth. Th/U ratios are 0.263 – 1.479 for inherited zircon cores, and 0.002 – 0.112 for, and almost indiscernible between, mantles and rims. Zircon mantles and rims from the Shawsheen Gneiss yielded a weighted mean 206Pb/238U age of 423 +/- 4.9 Ma (N = 32; MSWD = 0.96). Zircon mantles and rims from the Marlboro Formation yielded a weighted mean 206Pb/238U age of 365 +/- 2.9 Ma (N = 42; MSWD = 0.77). The crosscutting dike yielded a weighted mean 206Pb/238U age of 356 +/- 3.0 Ma (N = 9; MSWD = 0.88). Partial melting had ended by this time. Results from this study suggests an along-strike younging of partial melt from ~423 Ma in the northeast to ~365 Ma in the southwest along the southeastern NT. This is consistent with results from previous work in the northwestern and southern NT.