Decoupling of surface and subsurface sutures in the Dabie orogen and a continent-collisional lithospheric-wedging model: Sr-Nd-Pb isotopic evidences of Mesozoic igneous rocks in eastern China.

Reports on the decoupling of surface and subsurface sutures in the Dabie orogen and a continent-collisional lithospheric-wedging model. Differences of neodymium (Nd) and lead (Pb) isotopic compositions between Mesozoic mafic igneous rocks from the North China Block (NCB) and the South China Block (SCB); Subsurface suture between the NCB and SCB; Southward movement of subsurface suture in the Dabie-Sulu orogen.