• 责任者：Yang Xiangsheng (Hunan Academy of Geological Engineering Exploration ; Zhuzhou 412003 ; China)
• 刊名：Geophysical and Geochemical Exploration
• 出版年：2009
• 卷期：33(4)
• 关键词：电法勘探 ; electrical exploration ; 找水 ; water research ; 湖南 ; Hunan Province
• 页码：p.403-405
• 图表：3 illus., 3 refs.
• 分类号：1600
• issnNo：ISSN1000-8918
• isbnNo：CN11-1906/P

ARGIN: 0cm 0cm 0pt" class=MsoNormal>amily: 宋体" lang=EN-US>With the combined profile method, the author inferred the existence of NE-trending and WE-trending fault structures in the logistics base of the amespace prefix = st1 ns = "urn:schemas-microsoft-com:office:smarttags" />ace w:st="on">aceName w:st="on">HuanghuaaceName> aceName w:st="on">InternationalaceName> aceType w:st="on">AirportaceType>ace>, with the former fault structure displacing the latter one. An analysis of amily: 宋体">ρang=EN-US>_s variability suggests that there exists strong shattering at the compounding place of the fault structures, which is thus the ideal position for underground water accumulation. IP sounding revealed the depth of the karst segment and the water accumulation degree. Drilling test at the anomaly point determined by geophysical exploration shows that the outflow of water has reached over 2 ame="m3" SourceValue="0" HasSpace="True" Negative="False" NumberType="1" TCSC="0">000 m³/d.amespace prefix = o ns = "urn:schemas-microsoft-com:office:office" />