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新密煤田翟沟井田山西组煤层特征及聚煤环境分析
引用本文:崔金池,俎新许,张坤.新密煤田翟沟井田山西组煤层特征及聚煤环境分析[J].中国煤炭地质,2012(7):15-17,28.
作者姓名:崔金池  俎新许  张坤
作者单位:河南省地质矿产勘查开发局第二地质勘查院,河南许昌461000
摘    要:以新密煤田翟沟井田勘探资料为基础,对井田区域特征、山西组煤层特征和沉积环境进行分析。研究表明:山西组下段为以泥坪+泥炭沼泽+泥坪沉积序列为主的潮坪沉积,山西组上段为以弱还原环境河流作用为主的三角洲沉积体系,山西组聚煤环境为滨岸潮坪环境;山西组二。煤层层位稳定,煤层结构简单,煤层厚度为0.82-12.20m,一般3—5m,平均厚度3.84m,煤层厚度的变化是受沉积环境、后期冲刷作用及构造作用综合作用的结果。

关 键 词:翟沟井田  山西组    煤层  沉积环境  聚煤环境

Shanxi Formation Coal Seam Features and Coal-accumulation Environment Analysis in Zhaigou Minefield, Xinmi Coalfield
Cui Jinchi,Zu Xinxu and Zhang Kun.Shanxi Formation Coal Seam Features and Coal-accumulation Environment Analysis in Zhaigou Minefield, Xinmi Coalfield[J].Coal Geology of China,2012(7):15-17,28.
Authors:Cui Jinchi  Zu Xinxu and Zhang Kun
Institution:(The Second Geological Exploration Institute, Henan Province Bureau of Geology and Mineral Resources Exploration and Exploitation, Xuchang, Henan 461000)
Abstract:Based on exploration data in Zhaigou minefield, Xinmi coalfield carried out minefield regional characteristics, Shanxi Formation coal seam features and sedimentary environment analyses. The study has demonstrated that: the Lower Member of Shanxi Formation is a tidal flat of mainly mudflat + peat bog + mudflat sedimentary sequence, the Upper Member of Shanxi Formation is a delta sedimentary system of mainly fluviation in a weak deoxidation environment. Shanxi Formation coal-accumulation environment is in a littoral tidal fiat. Coal II1 in Shanxi Formation has a steady horizon; texture of coal seam is simple, coal thickness 0.82m-12.20m, generally 3m-5m, average 3.84m. Coal thickness variation is a result of combined actions of sedimentary environment, succeeding scouting and tectonic processes.
Keywords:Zhaigou minefield  Shanxi Formation  coal seam II1  sedimentary environment  coal-accumulation environment
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