低地和高地边界现今地形与古生代地台地质构造的关系——以波兰中部为例

IF 0.4 Q4 ENVIRONMENTAL SCIENCES Geology, Geophysics and Environment Pub Date : 2019-04-25 DOI:10.7494/GEOL.2019.45.1.57
A. Szmidt, Lucyna Wachecka-Kotkowska
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引用次数: 2

摘要

本文试图找出Łodź向斜、拉多姆斯科高地和贝尔查图夫地堑及其中部波兰低地和高地交界处现今地形的中生代地表地质与动力学之间的关系。化石浮雕已经与现在的浮雕进行了比较,因为它与萨利安(瓦塔尼亚)冰原衰退阶段的程度有关。发现中生代地表平原与主要地貌要素之间有明显的收敛。在前更新世和当代景观中,海拔和化石谷的作用被强调为稳定的形式。还强调了地堑和高地的意义,使中波兰冰期的瓦塔尼亚期停顿时间更长。
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Relations between present relief on the border of lowlands and highlands and geological structures of the Paleozoic Platform – a case study from central Poland
The article is an attempt to find relations between geology and the dynamics of the Mesozoic surface of the Łodź Synclinorium, the Radomsko Elevation and the Belchatow Graben and the present relief on the border of the Polish Lowlands and Uplands in its central part. Fossil relief has been compared with the present one as related to the extent of the recession phases of the Saalian (Wartanian) ice-sheet. A significant convergence has been found between the Mesozoic surface plain and the main morphologic elements. The role of elevations and fossil valleys has been stressed as stable forms in the pre-Pleistocene and contemporary landscape. Also stressed has been the meaning of grabens and elevations enforcing longer stoppages of the Wartanian stadial of the Middle Polish Glaciations.
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