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岩溶蓄水构造与找水 --以广西来宾小平阳为例

张之淦 陈伟海

水文地质工程地质2000,Vol.27Issue(6):1-5,5.
水文地质工程地质2000,Vol.27Issue(6):1-5,5.

岩溶蓄水构造与找水 --以广西来宾小平阳为例

ENGLISH

张之淦 1陈伟海1

作者信息

  • 1. 国土资源部岩溶地质研究所,桂林 541004
  • 折叠

摘要

Abstract

Eight groups of water-bearing structures for densely-consolideted and karstified paleozoic carbonate rocks in a plain area of Central Guangxi are given, which were formed in secondary dissolution process along tectonic fractures and paleokarst formations in an evironment of subtropical climate and the second tectonic subsidence zone during Cenozoic era in Eastern China. The quantitative characterization of their 3-dimensional geometry and void space texture may serve as geological basis for planning geophysical prospecting work and interpretation of its results. The structures occupy only 1%~10% of the volume of karst aquifers. Recognization of them by karstic hydrogeologic survey can reduce the target area by 1~2 orders of magnitute

关键词

岩溶/地下水/找水/广西

Key words

karst/groundwater/exploration/Guangxi

分类

天文与地球科学

引用本文复制引用

张之淦,陈伟海..岩溶蓄水构造与找水 --以广西来宾小平阳为例[J].水文地质工程地质,2000,27(6):1-5,5.

基金项目

广西留学回国人员科学基金(桂科回9661010)和地矿部“八五”重点攻关课题(85-01-009-01-1)共同资助 (桂科回9661010)

水文地质工程地质

OACSCD

1000-3665

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