【摘要】 界于东经 10 8°30′～ 110°,商丹带 -勉略带 (或大巴山带 )之间的山柞旬 -安康构造带是在古生代 -三叠纪南北向裂陷 -裂谷板内海相沉积盆地基础之上转化形成的 型造山带 ,它与东、西两侧的武当 -商南带、佛坪 -汉南带的组成、结构均不相同。南秦岭的山柞旬 -安康带开始从南向北以及后来再自北向南的两次逆冲推覆所形成的构造格局 ,与目前都认为该区是从北向南指向四川盆地的滑脱—逆冲式的薄皮构造模式是完全不同的。笔者还简要讨论了 型造山带的基本特征更多还原

【Abstract】 The Shanyang-Zhashui-Xunyang-Ankang tectonic belt lying in 108°30′～110°,and between Shangxian-Danfeng and Mianxian-Lueyang (or Dabashan) tectonic belts, is Ⅱ-type orogenic belt that was formed in Palaeozoic-Triassic by the transfomation from N-S trending intraplate oceanic sedimentary basin.It is different from Wudang-Shangnan tectonic belt to its east and Foping-Hannan tectonic belt to its west in the composition and structure.The tectonic pattern produced by over-thrusting from south to north at the beginning and the over-thrusting from north to south late in Shanyang-Zhashui-Xunyang-Ankang region of the South Qinling is completely from the thin-skinned structural model in which the region was slide-thrusted toward Sichuan basin from north to south.This paper also discussed the basic features of Ⅱ-type orogenic belt.更多还原