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安家岭井工矿二号井含煤岩系沉积环境

Anjialing Underground Coalmine No.2 Coal Measures Sedimentary Enviroment
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摘要 11号煤层直接沉积在潮坪和潮坪砂坝的隆起基底上,9号煤层亦发育在三角洲前缘的隆起区,成煤时间长,煤层厚度大,井田东部煤层最厚,薄煤带位于研究区南东角。8号和10号煤层为9号煤层在沉积过程中的局部分叉,而且分叉指向砂体和海,故9号煤层为岛状成煤条件。4^(-1)号煤层沉积在冲积平原的陆相环境。 The coal No. 11 has directly deposited on tidal flat and tidal flat sandbar uplifted basement; coal No. 9 also developed on delta front uplifted area. Since long coal-forming duration has caused large coal thickness. Thickest coal seams have developed in minefield eastern part,thin coal belt situated in southeast corner of the study area. Coal No. 8 and No. 10 are all local splits of coal No. 9 during the sedimentation,while the bifurcation directing on sand body and sea,thus the coal No. 9 should be deposited on an island.Coal No. 4(-1) was deposited on an alluvial plain with terrestrial environment.
作者 郄润来 Qie Runlai(Shanxi Provincial Coal Geological No.115 Exploration Institut)
机构地区 山西省煤炭地质
出处 《中国煤炭地质》 2018年第5期10-14,19,共6页 Coal Geology of China
关键词 砂体 岩石类型 煤层沉积环境 sand body rock type coal seam sedimentary environment
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