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青海绿草沟煤矿控煤断层特征及赋煤规律

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为进一步查明青海绿草沟煤矿控煤构造特征及赋煤规律,对绿草山地区已开展的地质工作进行整理分析,系统梳理该地区发育的7条控煤断层,详细总结了影响绿草沟煤矿主要可采煤层赋存的地质构造性质及控煤机理.结果表明,绿草沟煤矿大体以F3断层为界划分为东西2个控煤构造区块,东部区块地质构造程度为复杂,西部区块地质构造程度为中等.G3煤层为局部可采的中厚不稳定煤层;G2上、G2下煤层为中厚—巨厚煤层,在东西部区块分别为局部可采的不稳定煤层、较稳定煤层;G1煤层在区内大部分发育,中厚—厚层状,在东部和西部区块分别为大部分可采的不稳定、较稳定煤层;F煤层为发育在F1-F2断层带内局部可采的特厚不稳定煤层.
Coal-controlling structural characteristics and the coal-bearing law of Lücaogou coal mine in Qinghai Province
Through the collation and analysis of the geological work carried out in the Lücaoshan area,the seven coal-controlling faults developed in the Lücaoshan area were systematically sorted out,and the geological structure properties and coal-controlling mech-anism affecting the occurrence of the main mineable coal seams in the Lücaogou coal mine were summarized in detail.The results indi-cate that,The Lücaogou coal mine is divided into two coal-controlling structural blocks in the east and west,with the F3 fault as the boundary.The geological structure of the eastern block is complex,and the geological structure of the western block is medium.The G3 coal seam is a medium-thick and locally recoverable unstable coal seam;the G2 upper coal seam and the G21ower coal seam are medium-thick and extremely thick coal seams.In the eastern and western blocks,the G2 uppercoal seam is locally recoverable unstable coal seam and the G2 lower coal seam is locally recoverable relatively stable coal seam;the G1 coal seam is a medium-thick-thick coal seam developed in most of the region.In the eastern and western blocks,it is mostly recoverable unstable coal seam and relatively stable coal seam,respectively.The F coal seam is an extra-thick and locally recoverable unstable coal seam developed in the F1-F2 fault zone.

coal-controlling faultgeological structurecoal seamcoal-bearing lawLücaogou coal mine in Qinghai

刘腾、鲍文广、王雪莹

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青海煤炭地质一○五勘探队,青海 西宁 810001

青海煤炭地质勘查院,青海 西宁 810001

控煤断层 地质构造 煤层 赋煤规律 青海绿草沟煤矿

2024

地质学刊
江苏省地质调查研究院,江苏省地质学会,中国地质学会

地质学刊

影响因子:0.621
ISSN:1674-3636
年,卷(期):2024.48(3)