摘要
讨论官地水电站坝区存在的复杂化学成分的高水头承压水形成的地质控制因素。该区特定的地貌位置、岩体结构、裂隙的组合关系和地应力环境共同决定了本区承压水的形成、分布特征。
The geological factors controlling the confined water with high piezometric levels and complicated hydro-chemical components, discovered in the right bank slope of Guandi hydropower station dam site, are discussed in this paper. Its formation is determined by the geomorphological position, fractures combination and tectonic stress environments.
出处
《地质灾害与环境保护》
2002年第1期65-68,共4页
Journal of Geological Hazards and Environment Preservation
