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地质构造的多重性,系指同一地区在不同地质时期曾卷入不同的方式、方向的构造运动,因此,就这个地域来说,相对不同构造体系而言,所占据的地位或所扮演的角色不同, 其中还有一些构造形迹或构造单元为两个或两个以上的构造体系所共有,从而形成它们的多重性。显然,多重性的实质就是构造复合问题。常见的多重性构造现象有:多重性断裂;多重性地块;多重性构造带;构造带与地块复合四种。
Geological structure of the multiplicity, refers to the same area in different geological periods have been involved in different ways and directions of tectonic movement, therefore, in this area, relative to different tectonic system, the position occupied or the role played In addition, some of the structural features or structural units are common to two or more structural systems, so as to form their multiplicity. Obviously, the essence of multiplicity is to construct compound problems. Common phenomena of multiple structures include: multiple fractures; plots of plots; multiple structural zones; structural belt and plots of four.