Halotectonic and Thrusting Processes in the Spanish Pyrnees

比利牛斯山是阿尔卑斯时代的碰撞造山带， 沿着伊比利亚和欧洲板块的边界。 关联 冲断强烈影响沉积作用， 盐层形成了一套异常发达的构造 这取决于一个非常脆弱的层。 该项目旨在 解决与逆冲作用、晕- 构造和沉积事件。 结果适用于 许多碰撞造山带，其中存在盐层。

The Pyrenees are an Alpine-age collisional orogen located along the border of the Iberian and European plates. Associated thrusting strongly affected sedimentation and the presence of salt beds produced an unusually well-developed set of structure that depend on a very weak layer. This project is designed to address problems related to the interaction of thrusting, halo- tectonic and sedimentary events. Results will be applicable to many collisional orogens in which salt beds are present.