[1] Wonsuck Kim,Chris Paola.Long-period cyclic sedimentation with constant tectonic forcing in an experimental relay ramp[J].Geology,2007,35(4):331-334.
[2] O'Brien N R,Meyer H W,Reilly K,et al.Microbial taphonomic processes in the fossilization of insects and plants in the late Eocene Florissant Formation,Colorado[J].Rocky Mountain Geology,2002,37(1):1-11.
[3] Humphrey N F,Heller P L.Natural oscillations in coupled geomorphic systems:an alternative origin for cyclic sedimentation[J],Geology,1995,23(6):499-502.
[4] Gurel A,Kadir S.Palaeoenvironmental approach to the geology,mine-ralogy and geochemistry of an Early Miocene alluvial-fan to cyclic shallow-lacustrine depositional system[J].Clay Minerals,2010,45:51-75.
[5] Hinnov L A,Ogg J G.Cyclostratigraphy and the astr onomical time scale[J].Stratigraphy,2007,4:239-251.
[6] Kuiper K F,Deino A,Hilgen F J,et al.Synchro nizing rock clocks of Earth history[J].Science,2008,320:500-504.
[7] 龚一鸣,杜远生,童金南,等.旋回地层学:地层学解读时间的第三里程碑[J].地球科学——中国地质大学学报,2008,33( 4) :443-457. Gong Yiming,Du Yuansheng,Tong Jinnan,et al.Cyclostratigraphy:the third milestone of stratigraphy in understanding time[J].Earth Science-Journal of China University of Geoscience,2008,33(4):443-457.
[8] 孟祥化,葛铭.中朝板块层序事件演化[M].北京:科学出版社.2004. Meng Xianghua,Ge Ming,Sequence of the Sino-Korean plate event evolution[M].Beijing:Science Press,2004.
[9] 梅冥相.碳酸盐岩米级旋回层序的成因类型及识别标志[J].岩相古地理,1993,33(6):34-45. Mei Minxiang.Genetic types and identification marks of meter-scale cyclic sequences of carbonate[J].Lithofacies Palaeogeography,1993,33(6):34-45.
[10] Gurel A,Kadir S.Palaeoenvironmental approach to the geology,inera-logy and geochemistry of an Early Miocene alluvial-fan to cyclic shallow-lacustrine depositional system[J].Clay Minerals,2010,45:51-75.
[11] 吴智勇,姜衍文.全球旋回地层学述评[J].石油与天然气地质,1996,17(1):15-21. Wu Zhiyong,Jiang Yanwen.Comments on global cyclostratigraphy[J].Oil & Gas Gelolgy,1996,17(1):15-21.
[12] 梅冥相.碳酸盐台地的层序地层格架及旋回地层级次[J].岩相古地理,1992,30(2):44-50. Mei Minxiang.Sequence stratigraphic framework and cycle ground level times of Carbonate platform[J].Lithofacies Palaeogeography,1992,30(2):44-50.
[13] 梅冥相.苏巷辰硅酸盐异成因复合海平面变化旋回层序[J].桂林冶金地质学院学报,1994,15(2):145-153 Mei Minxiang.Differentiation cause composite sea level changes cyclic sequence of Portland of Suxiangcheng[J].Guilin Metallurgical Geological Institute,1994,15(2):145-153.
[14] Johnson C L,Graham S A.Cycles in perilacustrine facies of Late Mesozoic rift basins,Southeastern Mongolia[J].Journal of Sedimentary Research,2004,74(6):786-804.
[15] Gurel A,Kadir S.Palaeoenvironmental approach to the geology,mine-ralogy and geochemistry of an Early Miocene alluvial-fan to cyclic shallow-lacustrine depositional system[J].Clay Minerals,2010,45:51-75.
[16] 远光辉,操应长,王艳忠.东营凹陷民丰地区沙河街组四段—三段中亚段沉积相与沉积演化特征[J].石油与天然气地质,2012,33(2):277-286. Yuan Guanghui,Cao Yingchang,Wang Yanzhong.Sedimentary facies and their evolution of the 4th-middle 3rd members of Shahejie Formation in Minfeng area,Dongying Sag[J].Oil & Gas Geology,2012,33(2):277-286.
[17] 李文浩,张枝焕,昝灵,等.渤南洼陷北部陡坡带沙河街组砂砾岩有效储层物性下限及其主控因素[J].石油与天然气地质,2012,33(5):766-777. Li Wenhao,Zhang Zhihuan,Zan Ling,et al.Lower limits of physical properties and their controlling factors of effective coarse-grained clastic reservoirs in the Shahejie Formation on northern steep slope of Bonan subsag,the Bohai Bay Basin[J].Oil & Gas Geology,2012,33(5):766-777.
[18] 吴智平,李伟,任拥军,等.济阳坳陷中生代盆地演化及其与新生代盆地叠合关系探讨[J].地质学报,2003,77(2):280-285. Wu Zhiping,Li Wei,Reng Yongjun,et al.Basin evolution in the Mesozoic and superposition of Cenozoic basin in the area of the Jiyang depression[J].Acta Geologica Sinica,2003,77(2):280-285.
[19] 操应长,王建,高永进,等.济阳坳陷东营凹陷古近系红层——膏盐层沉积特征及模式[J].古地理学报,2011,13(4):375-386. Cao Yingchang,Wang Jian,Gao Yongjin,et al.Sedimentary characteristics and model of red beds—gypsum salt beds of the Paleogene in Dongying Sag,Jiyang Depression[J].Journal of Palaeogeography,2011,13(4):375-386.
[20] 谭先锋,田景春,李祖兵,等.碱性沉积环境下碎屑岩的成岩演化[J].地质通报,2010,4(20):6-14. Tan Xianfeng,Tian Jingchun,Li Zubing,et al.The diagenetic evolution clastic alkaline depositional environment[J].Geological Bulletin,2010,4(20):6-14.
[21] 谭先锋,田景春,李祖兵,等.东营凹陷古近系孔店组成岩特征及对储层的控制[J].煤田地质与勘探,2010,38(6):27-32. Tan Xianfeng,Tian Jingchun,Li Zubing,et al.Diagenetic character and controling factor of reservoir of Kongdian Formation of Paleogene in Dongying basin[J].Coal Geology & Exploration,2010,38(6):27-32.
[22] 黄思静,黄可可,冯文立,等.成岩过程中长石、高岭石、伊利石之间的物质交换与次生孔隙的形成[J].地球化学,2009,38(5):498-506. Huang Sijing,Huang Keke,Feng Wenli,et al.Mass ecchanges among feldspar,kaolinite and illite and their influences on secondary porosity formation in clastic diagenesis[J].Geochimica,2009,38(5):498-506.
[23] 刘志飞,赵玉龙,李建如,等.南海西部越南岸外晚第四纪粘土矿物记录:物源分析与东亚季风演化[J].中国科学(D辑),2007,37(9):1176-1184. Liu Zhifei,Zhao Yulong,Li Jianru,et al.Late Quaternary clay mineral record in the western south China Sea coast of Vietnam:source analysis and East Asian monsoon evolution[J].Science in China(D Series),2007,37(9):1176-1184.
[24] 应凤祥,罗平,何东博.中国含油气盆地碎屑岩储集层成岩作用与成岩数值模拟[M].北京:石油工业出版社,2004. Ying Fengxiang,Luo Ping,He Dongbo.Diagenesis and diagenetic numerical simulation of clastic reservoir of petroliferous basins in China[M].Beijing:Petroleum Industry Press,2004.
[25] 谭先锋,田景春,林小兵,等.陆相断陷盆地深部碎屑岩成岩演化及控制因素:以东营断陷盆地古近系孔店组为例[J].现代地质,2010,24(5):934-944. Tan Xianfeng,Tian Jingchun,Lin Xiaobing,et al.Diagenetic evolution and controling factors of deep-seated clastic rocks in terrestrial fault-depressed Basin[J].Geoscience,2010,24(5):934-944. |