厚皮变形（英语：Thick-skinned deformation）是指造成地壳缩短，并通常涉及基底岩层和深部断层的构造变形[1]。最常见的是在大陆碰撞区的造山运动地带。地壳不但水平向缩短并垂直向加厚。变形以褶皱和逆冲断层为主。但在高温下地壳流（英语：crustal flow）亦能发生[2]。
 |
参考文献
Wikiwand in your browser!
Seamless Wikipedia browsing. On steroids.
Every time you click a link to Wikipedia, Wiktionary or Wikiquote in your browser's search results, it will show the modern Wikiwand interface.
Wikiwand extension is a five stars, simple, with minimum permission required to keep your browsing private, safe and transparent.
