摘要
采用煤地质学、煤地球化学及沉积学方法,对枣庄陶枣煤田早二叠纪13、14和17煤层及底板黏土岩进行采样测试发现:不同煤层底板的黏土岩质量存在着差异,13、14煤为海退形成煤层,其黏土岩高岭石、伊利石含量相对较低,石英含量较高,形态多呈尖棱状。17煤是海侵形成,其黏土岩高岭石、伊利石含量相较高,石英含量较低,形态多为次圆状,化学风化指数(CIA)在84.26%~92.18%,平均为88.22%,受到的化学风化作用较弱,黏土质量更好;化学分析结果表明:研究区黏土岩SiO_2含量为40.61%~63.91%,Al_2O_3含量为21.52%~42.92%,碱金属及其他氧化物含量较低,且Fe_2O_3含量为0.48%~2.98%,TiO_2含量为0.31%~1.32%,在耐火材料工业达到一级品位,有利于深加工应用。该研究结果为煤系共伴生矿产开采提供了一定的依据。
Using coal geological, coal geochemical and sedimentological methods have carried out sampling and testing for early Permian coal Nos. 13, 14, 17 and floor claystone in the Taozao coalfield, Zaozhuang.. The result has shown that the quality of floor claystnne under different coal seams is different. Coal Nos. 13 and 14 were formed during regression, the claystone has relatively lower kaolinite and illite contents, higher quartz content, mostly sharp angular in shape. Coal No. 17 was formed during transgression, the claystone has relatively higher kaolinite and illite contents, lower quartz content, mostly subrounded in shape; the chemical weathering index ( CIA ) is between 84. 26% -92. 18%, average 88.22%, thus weaker chemical weathering, claystone quality is better. The chemical analyzed results have shown that study area claystone SiO2 content range between 40. 61% - 63.91%, AlO3 between 21.52% 42. 92% ; contents of alkali metals and other oxides are rather low, Fe2O3 between 0.48% -2. 98%, TiO2 between 0. 31% - 1.32% , thus the grade I in refractory industry, conducive to deep processing applications. The result has provided certain basis in coal meas- ures coexisting and associated minerals exploitation.
作者
张艺
吕大炜
Zhang Yi Lyu Dawei(College of Earth Science and Engineering, Shandong University of Science and Technology, Qingdao, Shandong 26659)
出处
《中国煤炭地质》
2017年第6期20-24,共5页
Coal Geology of China
基金
山东省自然科学基金(ZR2015JL016)资助
关键词
陶枣煤田
黏土岩
海侵
地球化学特征
Taozao coalfield
claystone
transgression
geochemical features