摘要
在现场水文地质调查的基础上,测试温泉水化学组成,研究其发育的地质环境和构造特征,分析温泉的形成条件和成因。结果表明该温泉受上塘复背斜和上塘-归龙断层控制,属断裂型温泉,呈带状分布。
Based on the field hydro-geological investigations, the hydro geochemical composition, geo-environment and geo- tectonics are studied to analyze the formation conditions and genesis of the spring. The result shows it is a rupture-typed spring of zonal distribution, influenced by Shangtang Anticlinorium and Shangtang-Guilong Fault.
出处
《地质灾害与环境保护》
2013年第1期47-51,共5页
Journal of Geological Hazards and Environment Preservation
关键词
贵州
温泉
构造
成因
Guizhou
thermal spring
tectonics
genesis
