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金庄陷落柱伴生黄泥带发育特征及成因探讨

evelopment Characteristics and the Causes of Wong Nai Belt Associated by Collapse Column in Jinzhuang

中文摘要英文摘要

为了探究金庄矿井下黄泥带的发育特征及成因,通过井上、下地质调查,采集岩样,进行全岩成分测试分析,综合研究黄泥带发育的影响因素,探讨其成因模式。结果表明:井下黄泥带的发育是陷落柱伴生的一种地质现象,以水平状产出,规模几百平方米至上千平方米,岩性主要为潮湿松软的泥状物质;岩样测试分析确定黄泥带的岩性为泥岩或泥质砂岩;其形成模式为:在地貌与构造的控水作用和陷落柱的导水作用下,地表水及地下水顺层入渗至9煤层中,在一定的条件下,9煤层顶、底板的泥岩或砂质泥岩被氧化成黄泥带。

In order to study the developmental characteristics and the genesis of the yellow ground under Jinzhuang mine , research the influence factors of yellow ground development comprehensively and discuss its genetic model, we can use ways of geological survey, collection sample and analysis of whole rock constituents of on and underground . Results show that the development of yellow ground is a geological phenomenon associated with collapse column , which is horizontal distribution ,the scale of hundreds of square meters to thousands of square meters and its lithology mainly is the soft damp gunk; the lithology of yellow ground is mudstone or argillaceous sandstone by sample test and analysis determining; the formation model is as follows: under the effect of water controlling of the landscape and construction as well as water guiding of collapse column, surface water and groundwater permeate through the 9 coal seam, under certain conditions, the mudstone or sandy mudstone of the 9 coal seam roof and floor is oxidized into yellow ground.

朱炎铭、王义海

矿山地质、矿山测量地质学矿业工程理论与方法论

地质学保利金庄煤矿岩溶陷落柱黄泥带成因模式

GeologyBaoli jinZhuang coal mineKarst collapse columnYellow groundGenetic model

朱炎铭,王义海.金庄陷落柱伴生黄泥带发育特征及成因探讨[EB/OL].(2013-04-27)[2025-08-28].http://www.paper.edu.cn/releasepaper/content/201304-562.点此复制

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