El paleomovimiento de Fonfría (Villablino, Cordillera Cantábrica)

Q4 Earth and Planetary Sciences

Geogaceta Pub Date : 2023-12-18 DOI:10.55407/geogaceta98194

Ángela Suárez Rodríguez, Augusto Rodríguez García, Rodrigo Castaño de Luis

引用次数: 0

Abstract

La cartografía geomorfológica permite clasificar el movimiento de ladera de Fonfría como un paleomovimiento paraglaciar, complejo e inactivo, al menos hasta el año 2000, en la fase previa a la explotación minera de carbón de Fonfría. Posteriormente, durante la fase de actividad minera y después, el movimiento empieza a ser afectado por estructuras de deformación gravitacional, reactivándose parcialmente.

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丰弗里亚古运动（坎塔布连山脉，比利亚布利诺）

通过地貌测绘，我们可以把丰弗里亚斜坡运动归类为副冰川古运动，至少在 2000 年之前，在丰弗里亚煤矿开采之前的阶段，这种运动是复杂而不活跃的。随后，在采矿活动阶段及其后，该运动开始受到重力变形结构的影响，部分重新活跃起来。

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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来源期刊

Geogaceta Earth and Planetary Sciences-Geology

CiteScore

0.40

自引率

0.00%

发文量

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