3.45 Ga granitic gneisses from the Yangtze Craton, South China: Implications for Early Archean crustal growth

Zircon U-Pb-Lu-Hf-O isotopic compositions of two granitic gneisses from the Kongling Terrain in the Yangtze Craton, South China were determined by SIMS, LA-ICP-MS and LA-MC-ICP-MS. Whole rocks of the two samples were analyzed for major and trace element compositions. The SIMS and LA-ICP-MS data reveal similar five zircon age groups of 3.4, 3.3, 2.9, 2.7, and 2.0 Ga for both gneisses. Three groups (magmatic Group A, metamorphic Group B, and overgrowth Group C) of the 3.4 Ga zircons were identified based on their CL images. These three groups have indistinguishable ages and Th/U ratios. Groups A and B show identical Hf-176/Hf-177 (t), although Group C was too thin to be analyzed by LA-ICP-MS. Taken together, zircons from the two samples with 98-102% age concordance give weighted average SIMS ages of 3434.3 +/- 9.6 Ma (2o-, MSWD = 13, n =8) for Group A, 3446.0 +/- 8.8 Ma (2a, MSWD = 10.7, 11 = 15) for Group B, and 3479 +/- 26 Ma (2o-,1VISWD = 0.49, n = 2) for Group C. Groups A and B together yield an upper intercept age of 3457 +/- 14 Ma (2o-, MSWD = 0.85, n=23). The LA-ICP-MS data yield weighted average ages of 3442 +/- 19 Ma (2a, MSWD =0.17, n = 7) for Group A and 3435 +/- 11 Ma (2a, MSWD = 0.44, n = 16) for Group B. They yield an upper intercept age of 3443 +/- 13 Ma (2 sigma, MSWD = 0.63, n = 23). These SIMS and LA-ICP-MS ages are consistent. We propose that the above SIMS and LA-ICP-MS ages of Groups A and B are the best estimates of the granitic magmatism and the subsequent metamorphism. The metamorphism must have occurred after the granitic magmatism within a few tens of million years, as constrained by their age errors. Accordingly, these two granitic gneisses represent the oldest rocks currently known in South China. They predate the previously reported 3300-Ma-old trondhjemitic gneiss from the Kongling Terrain by 150 Ma. The 3.4 Ga zircons show near chondritic sElf (t) (-0.7 1.0, 2a, MSWD = 1.14, n =8), which is below the coeval value of the depleted mantle. This suggests that the granitic magma contained materials of preexisting continental crust. Their higher-than-mantle 8180 values (6.1-6.4%) imply that such materials must have been interacted with surface water. Crust formation ages (TDDA2) of the 3.4 Ga zircons vary from 3.9 to 3.6 Ga with a weighted average of 3703 27 Ma (2a, MSWD = 1.05, n = 7). Our results support previous studies that the Yangtze Craton may have contained the continental crust as old as 3.8 Ga. Among the younger age groups, the 3.3 Ga zircons exhibit Hf-176/Hf-177 (t) and delta O-18 values similar to the 3.4 Ga zircons, suggesting that they were altered from the 3.4 Ga zircons. The 2.9 and 2.7 Ga zircons in both samples are rare and magmatic. Their Hf-176/Hf-177 (t) ratios are distinct from the 3.4 Ga zircons, indicating different sources. These two age groups are consistent with the 2.9 Ga trondhjemitic-tonalitic-granodioritic and the 2.7 Ga A-type granitic magmatism in the Kongling Terrain. The 2.0 Ga metamorphic zircons, regardless of being concordant or discordant, have Hf-176/Hf-177 (t) ratios overlapping those of the 2.7 Ga zircons, suggesting a common source. In contrast, delta O-18 of the 2.0 Ga zircons is strongly variable and positively correlated with age concordance. The low delta O-18 (down to 3.1%.) requires interaction with hydrothermal fluid. These results suggest that at least some of the 2.0 Ga zircons were likely to have been altered from the 2.7 Ga zircons by hydrothermal fluid. (C) 2014 Elsevier B.V. All rights reserved.