一、亚洲板块内构造应力场亚洲大陆的地质构造表现为前寒武纪地盾地台等各种时代的造山带的复杂特征。但是在目前,它们却互相连接一体,占据庞大的欧亚板块的东半部。欧亚板块的东缘与太平洋、菲律宾海板块相接,成为长大的汇聚型边界。其南缘与印度次大陆和阿拉伯板块相碰撞,形成包括喜马拉雅山脉在内的阿尔卑斯—喜马拉雅 First, the tectonic stress field in the Asian plate The geological structure of the Asian continent shows the complex features of orogenic belts in various epochs such as the Precambrian shield. But for now, they are interconnected and occupy the eastern half of the vast Eurasian plate. The eastern edge of the Eurasian Plate joins the Pacific Ocean and the Philippine Sea Plate and becomes the converging boundary that grows up. Its southern margin collided with the Indian subcontinent and the Arabian plate to form the Alps-Himalayas, including the Himalayas