摘要
青藏铁路将通过青藏高原连续多年冻土地区 ,高原多年冻土地区发育有特殊的不良地质现象 ,如厚层地下冰、热融滑坍、热融沉陷或热融湖 (塘 )、沼泽化湿地、冰锥、冰丘和爆炸性充水鼓丘、融冻泥流等。如果处理不当 。
The railway from Ge ermu to Lasa will cross the area of permafrost with many bad geological problems such as thaw slumping, thaw settlement, aufeis, and so on, which may bring about great many difficulties to Qinghai Tibet railway construction.
出处
《水文地质工程地质》
CAS
CSCD
2002年第1期45-48,共4页
Hydrogeology & Engineering Geology
