Active Faults in Iberia

J. J. Martínez-Díaz, E. Masana, M. Rodríguez-Pascua
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引用次数: 13

Abstract

The distribution of active faults in the Iberian Peninsula is not homogeneous, being mainly present, but not only, in areas affected by the Alpine Orogeny. They are located in several regions: (1) The Iberian Massif, including Portugal, and Galicia and Cantabrian Mountains in the North, (2) The Pyrenees, (3) The NE of Iberia, (4) The Iberian Cordillera, and (5) The Betic Cordillera. The Pyrenees, the Iberian Cordillera, and particularly the Betic Cordillera are the most active regions. These faults have being considered active in a broad sense, that is to say, corresponding to faults that, at least, present movements during the Quaternary, not restricting them only to those presenting displacements during the late 10,000 years. Although important, faults situated offshore have not being included in the present review.
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伊比利亚的活动断层
伊比利亚半岛活动断裂的分布不均匀,主要存在于受阿尔卑斯造山运动影响的地区,但不仅如此。它们分布在几个地区:(1)伊比利亚山脉,包括葡萄牙、加利西亚和北部的坎塔布连山脉;(2)比利牛斯山脉;(3)伊比利亚东北部;(4)伊比利亚山脉;(5)贝蒂亚山脉。比利牛斯山脉,伊比利亚山脉,尤其是贝蒂亚山脉是最活跃的地区。这些断层在广义上被认为是活跃的,也就是说,至少与第四纪期间出现运动的断层相对应,而不仅仅局限于那些在晚一万年中出现位移的断层。虽然重要,但位于海上的断层没有包括在本次审查中。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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Active Faults in Iberia Variscan Metamorphism The Alpine Orogeny in the West and Southwest Iberia Margins The Finisterra-Léon-Mid German Cristalline Rise Domain; Proposal of a New Terrane in the Variscan Chain Active Deformation in the Iberian Peninsula from Geodetic Techniques
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