Halotectonic and Thrusting Processes in the Spanish Pyrnees

西班牙比利尼山脉的晕构造和逆冲过程

• 批准号: 8816335
• 负责人: David Anastasio
• 金额: $ 7.97万
• 依托单位: Lehigh University
• 依托单位国家: 美国
• 项目类别: Continuing grant
• 财政年份: 1989
• 资助国家: 美国
• 起止时间: 1989-04-01 至 1991-12-31
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=8816335&HistoricalAwards=false
• 关键词: Halotectonic; Thrusting; Processes; Spanish; Pyrnees

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.

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、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。