Professor Zhang Haijiang from the School of Earth and Space Sciences, University of Science and Technology of China (USTC), in collaboration with academician Hou Zengqian from the Institute of Geology, Chinese Academy of Geological Sciences, and Professor Wang Qingfei from the China University of Geosciences (Beijing), have discovered that the lithosphere architecture characterized by crust-mantle decoupling controls the formation of orogenic gold belts. The research results were published in the National Science Review.
