摘要
The global tectonic regime underwent a major transition in the Mesozoic. Large-scale magmatic activities and mineralization occurred in China during this stage, known as the Yanshanian Movement, which is an important tectonic event that formed the present-day tectonic framework and topography of eastern China. It consists of two compressions and three extensions (Dong et al., 2018;Meng, 2017).
