十年后的ESCI-N项目:结果和开放问题的síntesis

G. F. Viejo, J. Gallastegui
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引用次数: 20

摘要

本文综合介绍了ESCI-N项目相关数据的结果和结论。ESCI-N项目始于上世纪90年代初,为Cantabrian山脉及邻近地区提供了第一套深反射和折射数据。在科迪勒拉山脉的最顶端发现了地壳根部,这标志着研究的一个突破点,在ESCI-N项目之后,坎塔布里亚科迪勒拉山脉和比利牛斯山脉之间的关系变得清晰起来。这些数据的研究和解释产生了重要的发现和新的约束,极大地改进了该地区的地球动力学和演化模型。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
The ESCI-N Project after a decade: A síntesis of the results and open questions
A synthesis of the results and conclusions from the data corresponding to the ESCI-N project is presented. The ESCI-N project developed in the early 90’s providing the first set of deep reflection and refraction data for the Cantabrian Mountains and adjacent areas. The discovery of a crustal root beneath the highest picks of the Cordillera marked a hit point on the studies and the relationship between the Cantabrian Cordillera and the Pyrenees became clear after the ESCI-N project. The study and interpretation of these data produced important findings and new constraints greatly improving the geodynamical and evolutional models of the area.
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