Historia geologiczna i współczesna rzeźba terenu /地质历史与当代浮雕

A. Michno
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引用次数: 0

摘要

考虑到基岩的年代和类型的多样性,本文介绍了该地区地质发展的主要阶段。论述了喀尔巴阡前深造山运动和高山造山运动的演化对Miechów盆地南部中新世构造发育和沉积的影响。讨论了气候变化和大陆冰川作用的发展对自然环境变化的影响:植被覆盖的变化、河流和斜坡沉积物的堆积以及地貌过程的强度。特别关注黄土盖层的形成——黄土的起源、年龄和沉积条件。在气候变化、聚落发展和人类经济活动的背景下,详细介绍了维斯瓦河谷底部和普罗佐维茨高原的地形发展。对该地区的当代地形特征、地貌过程的类型和强度进行了描述。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Historia geologiczna i współczesna rzeźba terenu / Geological history and contemporary relief
The text presents the main stages of the geological development of the area, taking into account the diversity of age and type of bedrock. The influence of evolution of the Carpathian Foredeep and Alpine orogenesis on the tectonic development and accumulation of Miocene sediments in the southern part of the Miechów Basin is presented. The impact of climate change and the development of continental glaciation on the transformation of the natural environment are discussed: changes in the plant cover, accumulation of fluvial and slope deposits, and the intensity of geomorphological processes. Particular attention is paid to the formation of loess cover – the origin of the loess, its age and deposition conditions. The development of the relief of the presented area – the bottom of the Vistula valley and the Proszowice Plateau – is presented in detail against the background of climate change, settlement development and human economic activity. The contemporary relief of the area as well as the type and intensity of geomorphological processes have been characterized.
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