济阳坳陷石炭—二叠系沉积特征及岩相古地理演化
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摘要
利用露头、钻井、地震和分析化验资料,依据沉积学基本原理和方法,对济阳坳陷石炭-二叠系沉积相及岩相古地理进行研究。结果表明:济阳坳陷石炭-二叠系沉积建造可以分为4种沉积体系和7类沉积相,即陆表海滨岸环境下台地-泻湖沉积体系、障壁岛-泻湖-潮坪复合沉积体系,海陆交互环境下的三角洲沉积体系以及陆相环境下的河流-湖泊复合沉积体系,发育泻湖、台地、潮坪、障壁岛、三角洲、河流和浅水湖泊等类型沉积相;受到华北板块周缘造山带影响,研究区古地理演化经历了由陆表海滨岸环境—海陆过渡相环境—陆相环境的转变。
By using sedimentology theories and outcrops,drilling,seismic and analytical and test data,sedimentary facies and lithofacies paleogeography of Pero-carboniferous system in Jiyang depression were studied.The results show that the sedimentary structure of the research area can be classified into four sedimentary systems including lagoon-platform sedimentary system,barrier land-lagoon-tidal flat sedimentary system,shallow delta sedimentary system,fluvial-lake sedimentary system and seven sedimentary facies including lagoon,plateau,barrier land,tidal flat,shallow delta,meandering river,shallow lake.Influenced by border orogenic belt of North China plate,the paleogeography evolved from epicontinental sea onshore environment,paralic environment to continental environment.
By using sedimentology theories and outcrops,drilling,seismic and analytical and test data,sedimentary facies and lithofacies paleogeography of Pero-carboniferous system in Jiyang depression were studied.The results show that the sedimentary structure of the research area can be classified into four sedimentary systems including lagoon-platform sedimentary system,barrier land-lagoon-tidal flat sedimentary system,shallow delta sedimentary system,fluvial-lake sedimentary system and seven sedimentary facies including lagoon,plateau,barrier land,tidal flat,shallow delta,meandering river,shallow lake.Influenced by border orogenic belt of North China plate,the paleogeography evolved from epicontinental sea onshore environment,paralic environment to continental environment.
引文
[1]李增学,刘华,余继峰,等.山东济阳坳陷石炭-二叠系煤成气储层沉积研究[J].沉积学报,2006,24(4):502-510.LI Zeng-xue,LIU Hua,YU Ji-feng,et al.Sedimentarystudy on coal-formed gas reservoir of Permo-Carboniferoussystem in Jiyang area,Shandong[J].Acta Sedimentolog-ica Sinica,2006,24(4):502-510.
[2]王力,金强,万丛礼,等.沾化凹陷孤北渤南地区深层天然气成因类型及其控制因素[J].中国石油大学学报:自然科学版,2008,32(5):35-40.WANG Li,JIN Qiang,WAN Cong-li,et al.Genetictypes and its controlling factors of deep natural gas in Gu-bei-Bonan area,Zhanhua depression[J].Journal of Chi-na University of Petroleum(Edition of Natural Science),2008,32(5):35-40.
[3]蒋有录.渤海湾盆地天然气聚集特征及形成条件[J].石油大学学报:自然科学版,1999,23(5):9-13.JIANG You-lu.Geological characteristics and formationconditions of the natural gas accumulation belts in Bohaibay Basin[J].Journal of the University of Petroleum,China(Edition of Natural Science),1999,23(5):9-13.
[4]DONALDSON A C.Pennsylvanian sedimentation of cen-tral appalachians[J].The Geol Soc of America SpecialPaper,1974,148(8):47-48.
[5]COLEMAN J M,PRIOR D B.Deltaic environment ofdeposition[M]//SCHOLLE P A,SPRARING D.Sand-stone geology.New York:McGraw-Hiu Book Co Inc,1982:137-138.
[6]葛宝勋,尹国勋,李春生.山西阳泉矿区含煤岩系沉积环境及聚煤规律探讨[J].沉积学报,1985,3(3):33-44.GE Bao-xun,YIN Guo-xun,LI Chun-sheng.Study ofcoal-bearing strata sedimentary environment and coal ac-cumulating pattern in Shanxi Yangquan mining area[J].Acta Sedimentologica Sinica,1985,3(3):33-44.
[7]陈世悦,徐凤银,刘焕杰.华北晚古生代层序地层与聚煤规律[M].东营:石油大学出版社,2000:18-36,99-112.
[8]曹忠祥,刘华,王玉林.济阳坳陷石炭-二叠系沉积与层序地层分析[J].山东科技大学学报:自然科学版,2002,21(2):68-72.CAO Zhong-xiang,LIUHua,WANG Yu-lin.Sedimenta-tion and stratigraphic sequence analysis of Permo-carbon-iferous system in Jiyang depression[J].Journal of Shan-dong University of Science and Techndogy(Natural Sci-ence),2002,21(2):68-72.
[9]王玉林.济阳地区上古生界沉积与层序地层分析[J].河南石油,2003,17(5):1-3.WANG Yu-lin.Sequence stratigraphic analysis on the up-per Palaeozoic in Jiyang area[J].Henan Petroleum,2003,17(5):1-3.
[10]李明娟,郑和荣,张海清.济阳坳陷晚古生代岩相古地理[J].石油地质与工程,2006,20(5):6-9.LI Ming-juan,ZHENG He-rong,ZHANG Hai-qing.Research on later Paleozoic lithofacies ancient geographyin Jiyang sag[J].Petroleum Geology and Engineering,2006,20(5):6-9.
[11]陈世悦.华北地块南部晚古生代-三叠纪盆地演化与盆山耦合关系研究[R].西安:西北大学,1997:112-170.
[12]陈世悦.论秦岭碰撞造山作用对华北石炭-二叠纪海侵过程的控制[J].岩相古地理,1998,18(2):48-54.CHEN Shi-yue.The controls of the collusion orogenesisin the Qinling Mountains on the Carboniferous-Permiantransgressional processes in North China[J].Sedimen-tary Facies and Palaeogeography,1998,18(2):48-54.
[2]王力,金强,万丛礼,等.沾化凹陷孤北渤南地区深层天然气成因类型及其控制因素[J].中国石油大学学报:自然科学版,2008,32(5):35-40.WANG Li,JIN Qiang,WAN Cong-li,et al.Genetictypes and its controlling factors of deep natural gas in Gu-bei-Bonan area,Zhanhua depression[J].Journal of Chi-na University of Petroleum(Edition of Natural Science),2008,32(5):35-40.
[3]蒋有录.渤海湾盆地天然气聚集特征及形成条件[J].石油大学学报:自然科学版,1999,23(5):9-13.JIANG You-lu.Geological characteristics and formationconditions of the natural gas accumulation belts in Bohaibay Basin[J].Journal of the University of Petroleum,China(Edition of Natural Science),1999,23(5):9-13.
[4]DONALDSON A C.Pennsylvanian sedimentation of cen-tral appalachians[J].The Geol Soc of America SpecialPaper,1974,148(8):47-48.
[5]COLEMAN J M,PRIOR D B.Deltaic environment ofdeposition[M]//SCHOLLE P A,SPRARING D.Sand-stone geology.New York:McGraw-Hiu Book Co Inc,1982:137-138.
[6]葛宝勋,尹国勋,李春生.山西阳泉矿区含煤岩系沉积环境及聚煤规律探讨[J].沉积学报,1985,3(3):33-44.GE Bao-xun,YIN Guo-xun,LI Chun-sheng.Study ofcoal-bearing strata sedimentary environment and coal ac-cumulating pattern in Shanxi Yangquan mining area[J].Acta Sedimentologica Sinica,1985,3(3):33-44.
[7]陈世悦,徐凤银,刘焕杰.华北晚古生代层序地层与聚煤规律[M].东营:石油大学出版社,2000:18-36,99-112.
[8]曹忠祥,刘华,王玉林.济阳坳陷石炭-二叠系沉积与层序地层分析[J].山东科技大学学报:自然科学版,2002,21(2):68-72.CAO Zhong-xiang,LIUHua,WANG Yu-lin.Sedimenta-tion and stratigraphic sequence analysis of Permo-carbon-iferous system in Jiyang depression[J].Journal of Shan-dong University of Science and Techndogy(Natural Sci-ence),2002,21(2):68-72.
[9]王玉林.济阳地区上古生界沉积与层序地层分析[J].河南石油,2003,17(5):1-3.WANG Yu-lin.Sequence stratigraphic analysis on the up-per Palaeozoic in Jiyang area[J].Henan Petroleum,2003,17(5):1-3.
[10]李明娟,郑和荣,张海清.济阳坳陷晚古生代岩相古地理[J].石油地质与工程,2006,20(5):6-9.LI Ming-juan,ZHENG He-rong,ZHANG Hai-qing.Research on later Paleozoic lithofacies ancient geographyin Jiyang sag[J].Petroleum Geology and Engineering,2006,20(5):6-9.
[11]陈世悦.华北地块南部晚古生代-三叠纪盆地演化与盆山耦合关系研究[R].西安:西北大学,1997:112-170.
[12]陈世悦.论秦岭碰撞造山作用对华北石炭-二叠纪海侵过程的控制[J].岩相古地理,1998,18(2):48-54.CHEN Shi-yue.The controls of the collusion orogenesisin the Qinling Mountains on the Carboniferous-Permiantransgressional processes in North China[J].Sedimen-tary Facies and Palaeogeography,1998,18(2):48-54.
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