Pb and Nd isotopic composition of the Jigongshan granite: constraints on crustal structure of Tongbaishan in the middle part of the Qinling-Tongbai-Dabie orogenic belt, Central China

The Qinling-Dabie-Sulu belt is the world's largest ultrahigh pressure (UHP) metamorphic belt. The UHP metamorphism is well dated at 220-245 Ma in the Dabie-Sulu belt but at similar to 507 Ma in the Qinling belt. The Tongbaishan is located between the Qinling orogenic belt to the west and the Dabie-Sulu UHP metamorphic belt to the east. It is the key area for studying the tectonic relation between the Qinling and Dabie-Sulu belts and the diachronous UHP metamorphism. The Jigongshan granitic pluton (t = 128 Ma) with a total area of 1200 km(2), composed of monzogramite, was mostly emplaced into the Tongbai complex, an exposed basement in the Tongbaishan. The Jigongshan granites have SiO2 = 69.85-72.35%, K2O/Na2O = 0.87-1.13, A/ CNK = 0.91 - 1.03, Rb/Sr = 0.14-0.25 and Th/U = 3.3-12. Their REE compositions show strongly fractionated patterns with (La/ Yb)(N) = 14-58 and Eu*/Eu = 0.79-1.05. The granites are characterized by low radiogenic Ph isotopic composition. The present-day whole-rock Pb isotopic ratios are Pb-206/Pb-204 16.707 - 17.055, Pb-207/Pb-204 = 15.239-15.326 and Pb-208/Pb-204 - 37.587-37.853, which are similar to that of the continental lower crust. Their epsilon(Nd)(t) values range from - 16 to - 20, and depleted-mantle Nd model ages (T-DM) from 1.8 to 2.2 Ga. The above evidence indicates that the magma of the Jigongshan granites was derived from the partial melting of the continental crust. The Ph and Nd isotopic compositions of the Jigongshan granites resemble those of the Dabie core complex in the Dabieshan but are distinct from those of the Tongbai complex in the Tongbaishan. Thus, the Dabie core complex would be the magma source of the Jigongshan granites. The result implies that the Dabie core complex is extended to the west and constitutes the unexposed basement underlaying the Tongbai complex in the Tongbaishan. (C) 2004 Elsevier B.V. All rights reserved.