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鲁西南石炭二叠纪煤系潮坪沉积体系与聚煤作用
引用本文:魏久传,李增学.鲁西南石炭二叠纪煤系潮坪沉积体系与聚煤作用[J].中国煤田地质,1995,7(3):25-30.
作者姓名:魏久传  李增学
作者单位:山东矿业学院地科系
摘    要:鲁西南石炭二叠纪煤系形成于内陆表海盆地。潮坪沉积体系是研究区聚时重要的沉积体系之一。作者详细研究了潮坪沉积体系的内部构成、成因相及各种沉积体发育特点,分析了沉积组合类型及其成因单元,论述了潮坪沉积体系的聚煤特点及富单元的形成与分布规律。

关 键 词:煤系  地层  沉积体系  聚煤作用  石炭纪  二叠纪

THE PERMO-CARBONIFEROUS TIDAL FLAT DEPOSITIONAL SYSTEM AND COAL-ACCUMULATION IN SOUTHWEST SHANDONG
Wei Jiuchran, LiZengxueL LiShouchun.THE PERMO-CARBONIFEROUS TIDAL FLAT DEPOSITIONAL SYSTEM AND COAL-ACCUMULATION IN SOUTHWEST SHANDONG[J].Coal Geology of China,1995,7(3):25-30.
Authors:Wei Jiuchran  LiZengxueL LiShouchun
Abstract:The Permo-carboniferous coal measures in Southwest Shandoug were formedin the North China epicontinental basin. Because of the specific characteristics of the basin-gentle slope and cast scope, the tidal flat may be regarded as an independent depositionalsystem. The paludification of tidal flat gives rise to the formation of important coalbeds.The authors give a detailed study ou the internal architecture,genetic facies of the deposi-tional system, analyse the sedimentary combination and their genetic units,go further intothe coal-accumulation and the formation and distribution of coal-rich wnits in the deposi-tioual system.
Keywords:Southwest Shandong  Coal measures  Tidal flat depositional system  Ge-netic facies  Sedimentary comhnation  Coal-accumulation:Coal-rich  unit
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