GEOCHEMICAL, AGE, AND ISOTOPIC CONSTRAINTS ON THE LOCATION OF THE SINO-KOREAN/YANGTZE SUTURE AND EVOLUTION OF THE NORTHERN DABIE COMPLEX, EAST CENTRAL CHINA
The Northern Dabie Complex (NDC) in east central China lies between the Sino-Korean plate to the north and the Yangtze plate to the south. It has been variously proposed to represent a Paleozoic magmatic arc on the Sino-Korean plate, an exhumed piece of subducted Yangtze plate crust, or crust produced almost entirely by Cretaceous extension-related magmatism. Trace element compositions of NDC orthogneisses and granites show arc signatures similar to those of UltraHigh-Pressure (UHP) rocks in the central Dabie, but no mineralogical evidence of UHP metamorphism is present in the samples investigated here. Field relationships, textures, compositions, and ion microprobe U-Pb zircon protolith crystallization ages reveal three distinct types of gneiss: diorite gneiss xenoliths (770 ± 26 Ma 95% confidence limit), within first generation highly deformed migmatitic grey gneisses (747 ± 14 Ma), cross-cut by second generation Cretaceous weakly foliated felsic gneisses (127 ± 4 Ma). Unfoliated Cretaceous granites (117 ± 11 Ma, monazite Th-Pb age=117 ± 1 Ma) intrude second generation gneisses. Cretaceous second generation gneisses and granites yield zircon inheritance ages of ~2 Ga, 700-800 Ma and (rarely) 227-271 Ma, indicating that the NDC is not simply a Cretaceous extensional terrane. The 700-800 Ma zircon ages are similar to those of granitic gneisses from the central UHP zone (698 ± 47 Ma) and are characteristic of the Yangtze craton. eNd values suggest that Cretaceous rocks in the NDC formed by partial melting of basement with very low eNd and not by melting of first generation or diorite gneisses. Nd depleted mantle model ages are consistent with the time of formation of the Yangtze craton at 1.4-2.5 Ga. The NDC is interpreted to be an extension of the Yangtze craton unaffected by UHP metamorphism. The Sino-Korean/Yangtze suture must lie to the north of the NDC.