摘要
内蒙古温都尔庙—白乃庙地区是早古生代中亚—蒙古海洋板块与华北陆台之间的海沟—岛弧体系。温都尔庙板块俯冲带的俯冲速度为5.38厘米/年。俯冲消减的深度达171.14公里,是一条超岩石圈的深断裂带.
The wenduermiao—Bailaimiao region in Inner Mongolia formed the trench—island is a system between the central Asian—Mongolia oceanic plate of Early palaeozoic and the North China continental platform. The subduction speed of the Wenduermiao subduction zone is 5.38 cm/year,and the extinction depth of this zone reaches 171.14kin,so this subduetion zone is a extra-lithospheric deep rift.
出处
《石家庄经济学院学报》
1985年第4期33-40,87,共9页
Journal of Shijiazhuang University of Economics
