利吉市基本地质地貌特征为空间规划的需要

M. Milivojević, Jelena Ćalić
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引用次数: 1

摘要

Ljig市位于塞尔维亚中部,位于潘诺尼亚盆地南缘的低山丘地区。本文通过列出的岩性要素,配以岩性图,概述了全市的地质组成,以及地下水含水层的基本类型(粒间层、裂隙层和岩溶层)。本文的地貌学部分提供了假设分析(海拔200至500米的丘陵地区占主导地位),以及地形暴露(西北、西部和北部暴露占主导地位),并附有相应的地图。除此之外,还有一个地形的遗传概况:它是由河流作用(优势类型)、山体运动和岩溶作用形成的。最后,对特定地貌单元的潜在利用进行了描述,并提出了切实可行的建议。优势河谷具有交通基础设施功能,丘陵有利于果树生长。在河谷坡面与冲积平原交界地区,滑坡是主要的限制因素。大多数河道的海鸥特征以及洪水的危险也是其局限性。
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Basic geological and geomorphological characteristics of Ljig municipality for the needs of spatial planning
Ljig municipality is situated in central Serbia, in the area of low hills at the southern rim of the Pannonian basin. The paper gives the overview of geological composition of municipal territory (through listed lithological elements, with lithological map), as well as the basic types of groundwater aquifers (intergranular, fissured and karstic). Geomorphological part of the paper offers the hypsometrical analysis (hilly areas at the altitudes from 200 to 500 m a.s.l. are dominant), as well as the relief exposures (northwestern, western and northern exposures are dominant), with the accompanying maps. Apart from that, there is a genetic overview of relief: it was formed by fluvial processes (dominant type), mass-movements, and karstic process. In the conclusion, the potential use of particular geomorphological units is described, with the practical suggestions. The dominant river valleys are in the function of transport infrastructure, while hills are favorable for fruit-growing. Landslides are the main limiting factor in the areas of contacts between valley slopes and alluvial plains. Gulling character of most river courses, as well as dangers from floods, are the limitations as well.
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