褶皱地带（fold belt，fold zones）简称褶带，是狭长带状、经历强烈地壳运动形成的构造地块。所有褶皱带都属于一定构造体系。
杉松岗钴（铜镍）矿床产于古元古代裂谷海槽褶皱地带，是国内新近发现的新类型矿床。它赋存于老岭群富硼、碳粘土岩夹硅质岩建造之中。
Shasonggang Co(Cu, Ni) deposit occurs in Laoling Group, rich boron, carbon clay rock with siliceous rock formation, Paleoproterozoic rift trough folded belt, which is the domestic a new type deposit.
但是在赤道地带以外地方，岩石会表现得富有弹性，常常起褶皱，就象正在放气的气球表面。
But outside of the equator, the rock behaves elastically and often bunches up, like the surface of a deflating balloon.
在地壳中一些柔弱地带往往较易受地壳运动剧烈而产生褶皱隆起，而造成绵亘的山脉，世界上许多山脉就是这样形成的。
In the crust some weak areas often more susceptible to intense crustal movement and fold uplift caused by stretching, the mountains, many of the world's mountains is formed.
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