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工程地质特征

  线路区属巴基斯坦东南部低山丘陵~冲洪积平原区,拟建路线基本沿印度河和哈布河两侧展布。沿线地形北东高、南西低,海拔高程多在30—500m之间,地形条件较为简单。

     The alignment area is located in the southeast Pakistan low mountains and hills - alluvial-proluvial plains, and the alignment extends basically along Indus River and Hub River. The terrain is high in the northeast part and low in the southwest part, with elevation almost between 30m and 500m. The topographic conditions are simple.

      区内地质构造发育程度不一,线路西南部为基岩出露区,地质构造复杂,断裂发育,剥蚀作用强烈,地貌形态属中低山—丘陵区;线路东部地质构造较为简单,为印度河冲洪积平原区,第四系松散岩类广泛分布,低洼地带有砂土、粉砂土及砂砾石土堆积,其间地表水系发育,辫状水系特征明显,遥感影像信息使人一目了然。

      The geological structure developed differently in the alignment area. The southwest region presents the rock outcrop and complex geological structure, with developed fracture and strong denudation, and the landform here belongs to low mountains and hills. The east region is on the alluvial-proluvial plain of Indus River, and has simple geological structure, with wide loose Quaternary rocks, and the sand, silty soil and sand and pebble deposit in the low-lying zone where the surface water system are developed. The braided water system is obvious, which can be observed clearly from remote sensing images.


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