摘要
本文以龙门山造山带为例，根据对阿尔泰—台湾地学断面地质学、地球物理学和地球化学等的综合研究，重点讨论了龙门山造山带岩石圈楔状构造的几何结构样式，探讨了碰撞后的陆内造山过程、造山模式及其科学意义。
Based on the synthetic study of geology, geophysics and geochemistry of the Altay-Taiwan geoscienpe traverse, this paper discussed emphatically the geometrical texture of lithospheric wedge structure in the Longmenshan origenic belt and explores the post-collision intracontinent orogenic process and model as well as its scientific significance.
出处
《四川地质学报》
1996年第2期97-102,共6页
Acta Geologica Sichuan
关键词
推覆构造
楔状构造
龙门山造山带
nappe structure, wedge structure, Longmensham orogenic belt
