摘要
含铵云母粘土岩夹矸较广泛分布于华北石炭二叠纪聚煤区太原组及山西组煤层中,其可划分为6种类型。文章详细描述了岩石的特征和铵云母在粘土岩夹矸中的赋存特点。测试结果表明铵云母均为1M型铵云母。它们是由成煤植物和有机质降解形成的NH4+离子,促使煤层粘土岩夹矸中的高岭石、伊利石在约120℃的酸性条件下转化成的。这种铵云母可以作为煤成气生成和储集的指示矿物。
he tobelite-bearing tonsteins are more widely distributed in the coal beds of Taiyuan and Shaxi Formation of .the Carboniferous-Permian coal mersures in Northern China,can be divided into the six rock types. Their lithological features and occurrences characteristices of the tobelites in the tonsteins are described in detail. The analytical results show that the tobelites are I M type. The tobelites are formed by alternating Kaolinite and Illite in the tonsteins under the effect of NH4+ formed by the degradation of coal forming plants and other organic substances, under the condition of acid medium, below 120℃. The tobelite can be regarded as a index mineral which forms and reserves the coal bed gas.
出处
《煤田地质与勘探》
CAS
CSCD
北大核心
1996年第3期11-16,T001,共7页
Coal Geology & Exploration
基金
煤炭部自然科学基金
关键词
地层
石炭纪
二叠纪
煤层
铵云母
粘土岩
tobelite
claystone
modes of presense
genesis
Carboniferous period
Permian period