褶皱带（fold belt）是指地槽中的沉积岩层经过剧烈的地壳运动后，由线型褶皱组合上升形成的强烈构造变形地带。在该地带内常伴有同造山期的大规模酸性岩浆侵入和广布的区域变质作用。
At the same time,the bituminous dikes also indicate the favorable foregrounds for exploration of Sinian-Cambrian oilfield in the east margin of fold belt of Longmen Mountain.
同时,矿山梁和碾子坝分布的沥青脉也指示在龙门山褶皱带东缘找寻我国最古老的震旦—寒武系油田的良好前景。
参考来源 - 川西北矿山梁地区沥青脉地球化学特征及其意义·2,447,543篇论文数据，部分数据来源于NoteExpress
第三种类型的山可能是由于火山活动形成的，一般发生在活动性褶皱带地区，如北美西部的喀斯喀特山脉。
A third type of mountain may be formed as a result of volcanic activity which occurs in regions of active fold mountain belts, such as in the Cascade Range of western North America.
甘孜-理塘断裂带是义敦造山带与雅江褶皱带的分界断裂。
Garze-Litang fracture zone separates Yidun orogenic belt from Yajiang folded belt.
文章对跨越大足重力高和龙门山褶皱带的重庆-黑水重力剖面作了解释。
The paper interprets the Chongqing-Heishui gravity profile traversing the Dazu high gravity gravity field and the Longmen Mountains fold belt.
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