摘要
在研究镜质组类型基础上,把富氢镜质组(荧光镜质体)作为有折扣的富氢显微组分(类脂组)对待,提出了利用荧光显微组分丰度——FMT 参数作为评价不同还原类型煤生烃、排烃的定量指标。煤岩学标志、有机地球化学参数和热模拟实验产烃率数据为 FMT 值定量评价煤生烃排烃潜力的适用性和有效性提供了佐证。
on the basis of type-vitrinite,authors think that perhydrous vitrinites(fluorescent vitrinite)should be considered discounted rich-hydrogen maceral(liptinite)and this is suggested that using“abundanceof fluorescent)macerals—FMT)”may be as quantitative index of hydrocarbon generation and expulsion ofcoals in different type-reductibility.Marks of coal petrology,parameters of organic geochemistry and yield-oil of thermal simulate--d experiment are provided evidence for availability of“FMT”evaluation method.
出处
《煤田地质与勘探》
CAS
CSCD
北大核心
1993年第6期18-22,共5页
Coal Geology & Exploration
基金
国家自然科学基金(编号:49070120A)
关键词
煤
生烃
排烃潜力
荧光显微组分
abudance of fluorescent macerals
evaluation
potentialies of hytrocarbon generation and expulsion