波兰低地Szczerców褐煤矿床的岩石组成

S. Pawelec, B. Bielowicz
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引用次数: 2

摘要

摘要对波兰低地Bełchatów褐煤矿Szczerców矿床褐煤的宏观和微观组成进行了研究。根据腐殖质煤的最新岩性分类,确定了其宏观组成。在此基础上,认为Szczerców矿床的主要岩型为泥质褐煤和木泥质褐煤。对11个褐煤样品进行了显微岩石组成测定。所检测的褐煤主要由腐殖岩群的矿物组成。其含量范围为75.2 ~ 86%,包括钠质岩(23.1 ~ 40.7%,平均28.9%)和致密岩(18.2 ~ 41.4%,平均24.9%)。研究还表明,褐煤中腐殖岩组矿物含量的统计变异性在所有样品中都很弱。另外,传统的测量方法是测量铝的随机反射率。结果为0.247 ~ 0.282%,最大允许标准差< 0.07。
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Petrographic composition of lignite from the Szczerców deposit, Polish Lowlands
Abstract Macroscopic and microscopic composition of lignite from the Szczerców deposit belonging to the Bełchatów Lignite Mine (Polish Lowlands) has been examined. The macroscopic composition was determined according to the newest lithological classification of humic coal. On this basis, it has been shown that the main lithotypes occurring in the Szczerców deposit are the detritic and xylodetritic lignites. The petrographic composition of the investigated lignite was determined microscopically for 11 samples. The examined lignite is predominantly composed of macerals from the huminite group. It is in the range from 75.2 to 86%, including atrinite (23.1–40.7%, averaging 28.9%) and densinite (18.2–41.4 %, averaging 24.9%). It also demonstrated that the statistical variability of the macerals content from the huminite group in the studied lignite is very weak in all samples. In addition, the random reflectance of ulminite was measured traditionally. The results, ranging from 0.247 to 0.282%, with the maximum permissible standard deviation < 0.07, were achieved for all analysed lignite samples.
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