单斜构造是指原来水平的岩层在受到地壳运动的影响后，产状发生变动。其中最简单的一种形式就是岩层向同一个方向倾斜，形成的构造。单斜构造往往是褶曲的一翼、断层的一盘或者是由局部地层的不均匀上升或下降所引起。
本文建立了内陆单斜构造内咸水入侵淡水含水层的三维可混溶溶质运移模型。
This paper presents a three-dimensional miscible solute transport model for salt water intrusion into fresh water aquifers, in an inland monoclinal structure.
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.
辽河盆地高升油田高81块为一东倾的单斜构造，其西北、西南、东南三面均为断层所限。
Gao no. 81 Block in Gaosheng Oilfield of Liaohe basin is a monocline structure plunging towards east, and its confined by faults in three directions of northwest, southwest and southeast.
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