南秦岭横丹浊积岩系是一套巨厚的浊流沉积，以向南或南东倾的单斜构造产出。
The Hengdan turbidite sequence is composed of very thick, normal turbidity current deposits. It is marked by a monocline dipping south or southeast.
另外，通过剑门关地区上侏罗统—下白垩统的磁化率各向异性研究发现，本区磁化率最大主轴方向可分为北东—南西向及北西—南东两组。
The study of magnetic susceptibility anisotropy in Jurassic and Cretaceous shows that there exit two maximal axis directions of magnetic susceptibility in the study area of Jianmenguan.
研究结果表明胜南6块构造高部位和胜南3东块为有利滚动区块。
The results of research show that preferable areas are higher position of structure in Shengnan 6 and eastern slope in Shengnan 3.
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