[1]毛邦燕,许模,白爱忠,等.广西合山煤田岩溶发育规律及机制研究[J].水土保持研究,2008,15(01):205-208.
　MAO Bang-yan,XU Mo,BAI Ai-zhong,et al.Study on the Karst Development Law and Mechanism of Heshan Coal Field in Guangxi Province[J].Research of Soil and Water Conservation,2008,15(01):205-208.
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广西合山煤田岩溶发育规律及机制研究

《水土保持研究》[ISSN:1005-3409/CN:61-1272/P] 卷: 15 期数: 2008年01期 页码: 205-208 栏目: 出版日期: 2008-02-20
Title:
Study on the Karst Development Law and Mechanism of Heshan Coal Field in Guangxi Province
作者:
毛邦燕1, 许模1, 白爱忠2, 黄润英3
1. 成都理工大学 地质灾害与环境保护国家专业实验室, 成都 610059;
2. 广西水文地质工程地质勘察院, 广西 柳州 545006;
3. 重庆煤田地质研究所, 重庆 400042
Author(s):
MAO Bang-yan1, XU Mo1, BAI Ai-zhong2, HUANG Run-ying3
1. National Laboratory of Geological Hazard and Engineering Geological Environment Protection, Chengdu University of Technology, Chengdu 610059, China;
2. Geological and Hydrogeological Surveying Institute Guangxi, Liuzhou, Guangxi 545006, China;
3. Geological Research Institute Coal field of Chongqing, Chongqing 401147, China
关键词:
合山煤田; 岩溶; 发育机制
Keywords:
Heshan coal field; Karst; development mechanism
分类号:
P642.25
摘要:
通过对合山煤田区119个钻孔揭露的溶洞数量、线溶洞率与高程之间的关系，地表岩溶出露的形态、位置、地下强径流带分布状况的研究，总结区内岩溶在垂向上和平面上的发育规律，并从区内岩石的物质基础、构造条件、水化学特征、水的循环交替作用等4个方面阐述区内岩溶的发育机制。结果表明：煤田区岩溶发育具有平面上的不均一性和垂向上的成层分布特征。前者体现岩溶在平面上发育受地层岩性、地质构造及水文地质条件等因素的影响；后者反映间歇性上升的新构造运动及侵蚀、溶蚀基准面和可溶岩出露厚度的变化对岩溶发育的控制。
Abstract:
The Karst development laws on the vertical and surface are determined through the analysis on the 119 holes data that it exposed the number of the cave, the relation of the line rate of cave and the elevation, the shape, location and the distribution of the strong strap radial flow, and explained the development mechanism of the Karst according to the rock material base, structure condition, hydrochemistry characteristic, and the function of the water circulation replace.The result of study shows: the Karst development has nonhomogeneity on the surface and layered distribution on the vertical.The former embodied the karst development is influenced by such factors as the stratum and rock, geological structure and hydrology geological condition factor etc.; And the latter reflected the intermission rises new tectonic movement, corroding and corrosion datum level, the change of the solvable rock’s emergence thickness controlled the karst development.

参考文献/References:

[1] 毛邦燕.复杂岩溶介质矿井涌水量的三维数值模拟研究[D].成都:成都理工大学, 2005.
[2] 沈继方, 李焰云, 徐瑞春.清江流域岩溶研究[M].北京:地质出版社, 1996:170-178.
[3] 李江.广西合山煤田区域岩溶发育规律及水文地质特征[J].广西煤田地质, 1990(1):2-12.
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备注/Memo

收稿日期:2006-9-19
作者简介:毛邦燕（1978- ），男，在读博士，主要从事工程地质、水文地质、环境地质研究。

更新日期/Last Update: 1900-01-01