[1] |
童晓光.中国东部早第三纪海侵质疑.地质论评,1985,31(3):261~267[Tong Xiaoguang.Doubts about the validity of Paleogene transgression in the eastern China.Geological Review,1985,31(3):261~267] |
[2] |
姚益民,徐金鲤,单怀广,等.山东济阳坳陷早第三纪海侵的讨论.石油学报,1992,13(2):29~34[Yao Yimin,Xu Jinli,Shan Huaiguang,et al.A discussion of the Paleogene transgression in the Jiyang Depression,Shandong Province.Acta Petrolei Sinica,1992,13(2):29~34] |
[3] |
汪品先. "海源陆生化石"与中国新生代"海侵"问题. 同济大学学报(自然科学版),1995,23(增刊):129~135[Wang Pinxian. Talassogenous fauna and "Cenozoic Transgressions" in China.Journal of Tongji University, 1985,23(Suppl):129~135] |
[4] |
孙镇城,杨藩,张枝焕,等.中国新生代咸化湖泊沉积环境与油气生成.北京:石油工业出版社,1997.69~303[Sun Zhencheng,Yang Fan,Zhang Zhihuan,et al.Sedimentary Environment and Hydrocarbon Generation of Cenozic salified Lakes in China.Beijing:Petroleum Industry Press,1997.69~303] |
[5] |
凌小惠.贵州二叠纪地层中海绿石矿物的发现及其地质意义. 矿物岩石,1985,3(5):96~107[Ling Xiaohui.The discovery and its geological significance of the glauconite in Permian strata in Guizhou Province. Minerals and Rocks,1985, 3(5) :96~107] |
[6] |
陈丽蓉,段伟民.生物状海绿石的成因.沉积学报,1987,3(5):171~177 [Chen Lirong ,Duan Weimin.Formation of glauconite as infillings of organism.Acta Sedimentologica Sinica, 1987,3(5):171~177] |
[7] |
金秉福, 林振宏,杨群慧,等.沉积矿物学在陆缘海环境分析中的应用.海洋地质与第四纪地质,2002,22(3):113~118[Jin Bingfu,Lin Zhenhong,Yang Qunhui,et al. Application of sedimentary mineralogy to the environmental analysis in marginal seas.Marine Geology & Quaternary Geology, 2002,22(3):113~118] |
[8] |
何镜宇,余素玉.黄骅坳陷北部古近系的海绿石.地球科学,1982,1(16):129~143[He Jingyu,Yu Suyu.Occurrence of glauconite in Lower Tertiary of Northern Huang-hua Depression.Earth Science, 1982,1(16):129~143] |
[9] |
刘德镒.黄骅坳陷古近系的沉积环境.矿物岩石,1985,3(5):109~115[Liu Deyi.Depositional environment of the eogene system in Huanghu Depression.Minerals and Rocks, 1985,3(5):109~115] |