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袁家矿区南段沉积环境与聚煤规律
引用本文:王小清,郑振华,刘珍奇. 袁家矿区南段沉积环境与聚煤规律[J]. 煤炭技术, 2009, 28(11)
作者姓名:王小清  郑振华  刘珍奇
作者单位:湖南省煤炭地质勘查院,湖南,长沙,410014
摘    要:根据钻孔资料,从岩性、层理、生物化石、煤层等特征分析袁家矿区南段含煤地层沉积环境和聚煤规律。结论为:含煤岩系地层是二叠系上统龙潭组;沉积环境为海陆过渡相;聚煤规律为早期滨湖-泻湖海湾环境、中期泻湖-湖沼环境和晚期滨湖三角洲环境等3个时期成煤。

关 键 词:龙潭组  沉积环境  聚煤规律  袁家矿区南段

Sedimentary Environment and Coal Accumulation Law of Southern Section of Yuanjia Mining Area
WANG Xiao-qing,ZHENG Zhen-hua,LIU Zhen-qi. Sedimentary Environment and Coal Accumulation Law of Southern Section of Yuanjia Mining Area[J]. Coal Technology, 2009, 28(11)
Authors:WANG Xiao-qing  ZHENG Zhen-hua  LIU Zhen-qi
Abstract:According to the drilling data,from the charactoristics of rock,bedding,fossils, coal seam est.features,analyzes the sedimentary environment and the coal accumulation law of the southern section of Yuanjia coal mining area.The conclusion is that the coal-bearing rock formation is the Permian Longtan group,the sedimentary environment is the sealand facres,the law of coal accumalation is the early lake-lagoon Gulf environment,the mid-lagoon-lake environment and late lake Delta environment est.three periods as coal formation.
Keywords:Longtan group  sedimentary environment  law of coal accumulation  southern section of Yuan mining area
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