| 萍-乐坳陷带之岩溶发育规律及岩溶水富集特征 |
| |
| 引用本文： | 张爱华.萍-乐坳陷带之岩溶发育规律及岩溶水富集特征[J].火山地质与矿产,2010(2):149-156. |
| |
| 作者姓名： | 张爱华 |
| |
| 作者单位： | 江西省地质调查研究院,江西南昌330030 |
| |
| 基金项目： | 中国地质调查局“萍乐坳陷带水文地质环境地质调查”（项目编码：1212020733905）资助.衷心感谢楼法生教授级高级工程师、魏源教授级高级工程师为提高本文质量所作的技术性指导. |
| |
| 摘 要： | 萍-乐坳陷带为江西省最主要的隐伏岩溶发育区带之一，岩溶地层发育，地表水、地下水循环交替强烈，地质构造复杂，为岩溶的发育、岩溶地下水的富集提供了良好的条件。查明岩溶发育规律及岩溶水的富集特征，可为地下水资源合理开发与地质环境保护提供科学依据。
|
| 关 键 词： | 岩溶 发育规律 岩溶水 富集特征 萍——乐坳陷带 |
Development pattern of karst and enrichment characteristics of karst water in Pingxiang-Leping depression belt |
| |
| ZHANG Ai-hua.Development pattern of karst and enrichment characteristics of karst water in Pingxiang-Leping depression belt[J].Volcanology & Mineral Resources,2010(2):149-156. |
| |
| Authors: | ZHANG Ai-hua |
| |
| Institution: | ZHANG Ai-hua (Geological Research Institute of Jiangxi Province, Nanchang, Jiangxi 330030) |
| |
| Abstract: | Pingxiang-Leping depression belt is one of the main development zones of blind karst in Jiangxi Province, where karst strata are well-developed, cycling and alternating of surface water and groundwater are strong and geological structures are complicated, providing favorable conditions for development of karst and enrichment of karst groundwater. To investigate development pattern of karst and enrichment characteristics of karst water may provide scientific basis for rational exploitation of groundwater resources and geological environmental protection. |
| |
| Keywords: | karst development pattern karst water enrichment characteristics Pingxiang-Leping depression belt |
| 本文献已被 维普 等数据库收录！ |
