山东莱芜盆地古近系大汶口组含水层找水实例分析-以口镇官水河村为例
投稿时间:2020-03-15  修订日期:2020-03-15  点此下载全文
引用本文:
摘要点击次数: 25
全文下载次数: 0
作者单位E-mail
周乐 中国地质调查局水文地质环境地质调查中心 zhoule_wei@sina.com 
朱庆俊 中国地质调查局水文地质环境地质调查中心 1969zhuqj@163.com 
罗旋 中国地质调查局水文地质环境地质调查中心  
李凤哲 中国地质调查局水文地质环境地质调查中心  
李伟 中国地质调查局水文地质环境地质调查中心  
刘元晴 中国地质调查局水文地质环境地质调查中心  
中文摘要:莱芜盆地内广泛分布大厚度古近系大汶口组砂泥岩地层,传统认识单井涌水量小于100 m3/d,长期作为弱富水含水层形式出现,不具有供水意义,特别是口镇-方下“长埠岭”地区,第四系厚度薄,水资源匮乏。本文结合中国地质调查局在口镇官水河村施工的探采结合孔,对高密度电阻率法在贫水古近系地层找水中的作用进行实例分析,以期为今后同类型地下水勘查提供借鉴。
中文关键词:高密度电阻率  大汶口组  水文地质  鲁中山区
 
Case study of water exploration in Dawenkou formation aquifer of Paleogene in Laiwu basin, with an example of Guanshuihe village, Kouzhen, Shandong Province
Abstract:The sandstone and mudstone strata of Dawenkou formation of Paleogene with large thickness are widely distributed in Laiwu Basin. Traditionally, the Dawenkou aquifer single well water inflow is less than 100 m3 /d, which has no water supply significance as a form of weak rich water aquifer for a long time. Especially in the "changbuling" area between Kouzhen and Fangxia, where the quaternary system is thin and lack of water resources. In this paper, through the exploration and mining combined hole constructed by China Geological Survey in guanshuihe village, Kouzhen. The application of high-density resistivity method in water exploration of water poor Paleogene strata is analyzed, in order to provide reference for the exploration of the same type of groundwater in the future.
keywords:High density resistivity  Dawenkou formation aquifer  hydrogeology  central mountain area of Shandong Province
  查看/发表评论  下载PDF阅读器
设备展厅
您是第7263790位访问者  备案许可证编号:京ICP备13036454号
版权所有:《中国矿业》杂志社有限公司
地  址: 北京市朝阳区安定门外小关东里10号院东小楼 邮编:100029 电话:010-68332570 88374940 E-mail: zgkyzzs@163.com