北秦岭为一复杂构造带，形成向北反转的叠瓦状逆冲推覆构造。
The north Qinling is a complicated structural zone, forming an imbricated thrust napped structure overturning northward.
北秦岭侵入岩带与同时代的蛇绿岩带有力地证明，北秦岭晋宁运动的构造体制是板块体制。
The intrusive rock belt and the ophiolite belt of the same time together demonstrate that the tectonic system of the North Qinling during the Jinning movement is plate tectonic system.
南秦岭新生代房县盆地是北西向安康竹山房县左旋走滑断裂构造带东南端拉分盆地。
The Fangxian basin of Cenozoic era of south Qinling is a pull-apart basin at the southeastern end of the Ankang-Zhushan-Fangxian NW-trending left-lateral strike-slip fault zone.
南秦岭新生代房县盆地是北西向安康竹山房县左旋走滑断裂构造带东南端拉分盆地。
The Fangxian basin of Cenozoic era of south Qinling is a pull-apart basin at the southeastern end of the Ankang-Zhushan-Fangxian NW-trending left-lateral strike-slip fault zone.
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