试论陆内型造山作用──以秦岭－大别山造山带为例  

AN INTRACONTINENTAL-TYPE OROGENY──Evidence from Qinling-Dabie Orogenic Belt,China

作　　者：赵宗溥[1] 

机构地区：[1]中国科学院地质研究所

出　　处：《地质科学》1995年第1期19-28,共10页Chinese Journal of Geology(Scientia Geologica Sinica)

摘　　要：板块构造学说的大陆碰撞作用和槽台学说的地槽回返作用不能解释秦岭－大别山造山带的成因机制。壳幔拆离构造导致陆内Ａ型俯冲是陆内型造山作用的成因机制。his paper mainly demonstrates that the causal mechanism of Qinling-Dabie Orogenic Belt could not be explained both by continental collision of plate-tectonics theory and by geosyncline inversion of the geosyncline-platfrom theory. Moreover,the author proposes that the crust-mantle detachment lead to the A-type subdution can interprete the causal mechanism of the Qinling-Dabie Orogenic Belt.

关 键 词：秦岭-大别山 造山带 陆内型 造山作用 

分 类 号：P542.2[天文地球—构造地质学]