摘要
通过收集大量钻孔资料,编制并分析了倾向沉积断面图、走向沉积断面图以及砂体等厚图。在此基础上,结合岩石成因标志和垂向层序,识别出元宝山组主要沉积相类型有:冲积扇相、湖泊相、扇三角洲相及河流相。然后,分析了其沉积环境演化,即经历了冲积扇—湖泊—扇三角洲—河流的演化过程。最后,阐述了元宝山组的聚煤规律。
Authors draw and analyze depositional trend and strike sections and sandstone isopach maps by collecting a lot of bores. Based on this, Four types of facies are identified that are alluvial fan facies, lacustrine facies, fan-deha facies and fluvial facies by studying petrous formation symbols and vertical sequences. Afterward evolvement of sedimentary environment is analyzed that is from alluvial fan to lacustrine to fan-delta to fluvial. In the end coal accumulation of Yuanbaoshan formation is expounded.
出处
《科学技术与工程》
2007年第10期2326-2330,共5页
Science Technology and Engineering
关键词
沉积环境
沉积相
聚煤规律
sedimentary environment sedimentary facies coal accumulation