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我国中部的秦岭-大别造山带是由华北地台和扬子地台在三叠纪碰撞而形成的。大别造山带的超高压变质作用及其地球动力学问题吸引了众多国内外地球科学家的广泛兴趣。
The Qinling-Dabie orogen in central China was formed by the collision of the North China Platform and the Yangtze Platform in the Triassic. The UHP metamorphism and its geodynamic problems in the Dabie orogen have attracted a great deal of interest from many earth scientists both at home and abroad.