ISSN 1006-3021 CN11-3474/P
Published bimonthly started in 1979
地球化学模拟在南北古脊梁岩溶裂隙水系统划分中的应用
  
关键词:Northward Archaic uplift  karst fissure water  geochemical modeling
基金项目:地质调查项目“宁南水资源综合评价与合理开发利用”(编号:DKD2002005-1)
作者单位E-mail
余秋生 中国地质大学,北京100083
宁夏地质工程勘察院,宁夏银川750021 
11998910@sina.com 
张发旺 中国地质科学院水文地质与环境地质研究所,河北石家庄050061  
韩占涛 中国地质科学院水文地质与环境地质研究所,河北石家庄050061  
于艳青 中国地质大学,北京100083
宁夏地质工程勘察院,宁夏银川750021 
 
薛忠岐 中国地质大学,北京100083
宁夏地质工程勘察院,宁夏银川750021 
 
摘要点击次数: 2596
全文下载次数: 2020
摘要:
Application of Geochemical Modeling in the Plotting of Karst Fissure Water Systems in the North-south Archaic Uplift, Ningxia, China
      Northward archaic uplift is the central part of Helan Mountain Northward tectonic system, it′s a uplift of Sinian, Cambrian, and Ordovician stratums. There is abundant karst fissure water in the limestone and dolomite of Cambrian and Ordovician. For the reason of deep embedding and complex tectonic condition, scatter and flow condition of the karst fissure water is still obscure. In this paper, geochemical modeling method was used to fix the border between karst fissure water systems and the relationship of diffe(rent) systems. The modeling results show that: the border between karst fissure water systemⅠandⅡ is between Yanwan and Lvtao, the border is a moveable groundwater dividing crest, and is recharged by quaternary groundwater; There is maybe strong groundwater flow along a water conductive fault between Sun spring and Mengcheng spring, about 46% of the groundwater of Sun spring is from Mengcheng spring by the connection of this water conductive fault.
YU Qiu-sheng,ZHANG Fa-wang,HAN Zhan-tao,YU Yan-qing,XUE Zhong-qi.2005.Application of Geochemical Modeling in the Plotting of Karst Fissure Water Systems in the North-south Archaic Uplift, Ningxia, China[J].Acta Geoscientica Sinica,26(4):375-380.
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