首页> 外文会议>Proceedings of international symposium on rock mechanics and mine dynamic disaster prevention >Development Characteristics of Coal-bearing Sand Body in South-central of Tiefa Mining Area——Both on the Prediction about Lithologic of Coal Seam Roof and Erosion Zone in Coal Seam
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Development Characteristics of Coal-bearing Sand Body in South-central of Tiefa Mining Area——Both on the Prediction about Lithologic of Coal Seam Roof and Erosion Zone in Coal Seam

机译:铁法矿区中南部含煤砂体的发育特征-兼论煤层顶板岩性和煤层侵蚀带预测

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摘要

With the application of phase analysis method,coal-bearing sand body in south-central of Tiefa mining area is divided into genetic types of anastomosed channel and braided channel sand body.Thus it reveals the respective characteristics of the two types of sand body.In sedimentary section diagram of anastomosed river,anastomosed channel sand body is surrounded by siltstone and claystone ;on the sand body thickness contour map,the high value area of anastomosed channel sand body is interwoven mesh;anastomosed channel sand body is located in the lower part of the sequence of the anastomosing river,the granularity of which is thinner upward.In sedimentary section diagram of braided river,the fine clastic rocks of the flood basin deposition are not developed surrounded by braided channel sand body;on the sand body thickness contour map,the high value area of the braided channel sand body shows the small camber width bebraided river channel sand body constitute the main body of braided river facies sequence,the granularity of which is thinner upward.On the basis,the No.15 coal points out that the coal seam roof is made up of anastomosed channel sand body in addition to the southeastern anastomosed channel sand body,the extent of which is nearly SN ;the anastomosed channel sand of the coal seam roof in other area is in NE extension as a whole.Erosion zone in coal seam is mainly located in the high value zone of the coal roof sand body.
机译:通过相分析方法的应用,将铁法矿区中南部的含煤砂体分为吻合河道和辫状河道砂体的成因类型,从而揭示了这两种类型砂体的各自特征。吻合河的沉积剖面图,吻合河道砂体被粉砂岩和黏土包围;在砂体厚度轮廓图上,吻合河道砂体的高价值区域是交织的网格;吻合河道砂体位于河床下部。在辫状河的沉积剖面图中,没有形成辫状河道砂体包围的洪水盆地沉积的细碎屑岩;在砂体厚度等值线上,辫状河道砂体的高价值区域显示出较小的弧度宽度带;辫状河道砂体构成了辫状河的主体序号越细,粒度越细。在此基础上,第15号煤层指出,煤层顶板除东南部吻合河道砂体外,还由吻合河道砂体组成。接近SN;其他区域煤层顶板的吻合河道砂总体上呈NE向延伸。煤层侵蚀带主要位于煤顶层砂体的高价值区。

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