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北京房山岩溶区节理裂隙分布特征研究

杨楠 李世君 孙颖 张院 许苗娟 黄煜琪

城市地质Issue(1):30-32,3.
城市地质Issue(1):30-32,3.

北京房山岩溶区节理裂隙分布特征研究

Study on Characteristics of Joints and Fissures in Karst Region of Fangshan, Beijing

杨楠 1李世君 2孙颖 1张院 3许苗娟 3黄煜琪3

作者信息

  • 1. 北京市地质工程勘察院,北京 100048
  • 2. 北京超维创想信息技术有限公司,北京 100085
  • 3. 北京市水文地质工程地质大队,北京 100195
  • 折叠

摘要

Abstract

Karst landform is widely developed in Fangshan, and we find that most joints and fissures measured here are nearly vertical;2~3 groups of joints and fissures are measured at one site which shows that it has large density with less filler through the statistical analysis of joints and fissures. Multiple sets of joints and fissures with the characters of high angles, high density, high penetrability are easy to be karstification and weathering. At the same time, the rain infiltration along original joints and fissures makes the fracture network expanded.

关键词

节理裂隙/房山/岩溶水

Key words

Joints and fissures/Fangshan/Karst water

分类

天文与地球科学

引用本文复制引用

杨楠,李世君,孙颖,张院,许苗娟,黄煜琪..北京房山岩溶区节理裂隙分布特征研究[J].城市地质,2014,(1):30-32,3.

基金项目

支持北京市岩溶水资源勘查评价工程,项目编号BJYRS-ZT ()

城市地质

2097-3764

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