山西省阳泉新景煤矿15煤微量元素的富集及沉积环境研究Study on Coal No. 15 Trace Elemental Enrichment and Sedimentary Environment in Xinjing Coalmine,Yangquan,Shanxi Province
岳琼申,丁典识,汪文军,周慧慧,刘桂建
摘要(Abstract):
在对山西省阳泉矿区中新景煤田15号煤层采集的30个煤样进行ICP-MS微量元素含量分析测试的基础上,讨论了新景矿15号煤层剖面上Li、Be、Sc、Cu、Ba、Sr、Rb、U、Th和Pb微量元素的分布和富集特征,发现15号煤中Li富集,Be,Sc,Rb亏损。通过计算Sr/Ba、Sr/Cu和U/Th比值作为判断成煤环境的地球化学指标,分析新景矿15号煤层的成煤环境。
关键词(KeyWords): 煤;微量元素;环境;阳泉矿区;新景矿
基金项目(Foundation): 本项目由国家自然科学基金(41672144)资助
作者(Author): 岳琼申,丁典识,汪文军,周慧慧,刘桂建
参考文献(References):
- [1]焦希颖,王一,等.阳泉矿区含煤地层沉积环境及其对煤层厚度分布控制[J].岩相古地理,1999,19(3):30-39.
- [2]朱英战.阳泉矿区矿井煤层气利用发展现状[J].煤炭科学技术,2013,41(10):70-72.
- [3]Zheng Q,Shi S,Liu Q,et al. Modes of occurrences of major and trace elements in coals from Yangquan Mining District,North China[J].Journal of Geochemical Exploration,2017,175:36-47.
- [4]葛宝勋,尹国勋,李春生.山西阳泉矿区含煤岩系沉积环境及聚煤规律探讨[J].沉积学报,1985(3):36-47.
- [5]吴占彩,贺克升.山西阳泉岩样稀土元素特征及其地质意义研究[J].山西焦煤科技,2010,34(12):15-18.
- [6]Dai S F,Zhou Y P,Ren D Y,et al. Geochemistry and mineralogy of the Late Permian coals from the Songzao Coalfield,Chongqing,southwestern China[J]. Science in China,2007,50(5):678-688.
- [7]Dai S,Li D,Chou C L,et al. Mineralogy and geochemistry of boehmite-rich coals:New insights from the Haerwusu Surface Mine,Jungar Coalfield,Inner Mongolia,China[J]. International Journal of Coal Geology,2008,74(3):185-202.
- [8]Ren D,Zhao F,Wang Y,et al. Distributions of minor and trace elements in Chinese coals[J]. International Journal of Coal Geology,1999,40(2-3):109-118.
- [9]Ketris M P,Yudovich Y E. Estimations of Clarkes for Carbonaceous biolithes:World averages for trace element contents in black shales and coals[J]. International Journal of Coal Geology,2009,78(2):135-148.
- [10]Taylor S R. Abundance of chemical elements in the continental crust:Amended basaltic rare earth patterns[J]. Geochimica Et Cosmochimica Acta,1965,29(2):145-146.
- [11]Valkovic,V. Trace elements in coal[M]. Boca Raton:CRC Press,1983.
- [12]Dai S,Seredin V V,Ward C R,et al. Enrichment of U–Se–Mo–Re–V in coals preserved within marine carbonate successions:geochemical and mineralogical data from the Late Permian Guiding Coalfield,Guizhou,China[J]. Mineralium Deposita,2015,50(2):159-186.
- [13]刘刚,周东升.微量元素分析在判别沉积环境中的应用———以江汉盆地潜江组为例[J].石油实验地质,2007(03):307-310+314.
- [14]王爱华.不同形态锶钡比的沉积环境判别效果比较[J].沉积学报,1996,14(4):168-173.
- [15]熊小辉,肖加飞.沉积环境的地球化学示踪[J].地球与环境,2011,39(3):405-414.
- [16]曲星武,王金城.用锶钡比研究沉积环境的初步探讨[J].煤田地质与勘探,1979(1):18-24.
- [17]王随继,黄杏珍.泌阳凹陷核桃园组微量元素演化特征及其古气候意义[J].沉积学报,1997,15(1):65-70.
- [18]Adams J A S,Osmond J K,Rogers J J W. The geochemistry of thorium and uranium[J]. Physics&Chemistry of the Earth,1959,3(3):298-348.
- [19]范玉海,屈红军,王辉,等.微量元素分析在判别沉积介质环境中的应用———以鄂尔多斯盆地西部中区晚三叠世为例[J].中国地质,2012,61(2):382-389.
- [20]钱利军,陈洪德,林良彪,等.四川盆地西缘地区中侏罗统沙溪庙组地球化学特征及其环境意义[J].沉积学报,2012,30(6):1061-1071.
- [21]莱尔曼,王苏民.湖泊的化学地质学和物理学[M].北京:地质出版社,1989.
- [22]邓宏文,钱凯.沉积地球化学与环境分析[M].兰州:甘肃科学技术出版社,1993.