GE Rui-quan. Occurrence and Geological Significance of Glauconite in Cenozoic Group of Jiyang Depression[J]. Acta Sedimentologica Sinica, 2004, 22(2): 276-280.
Citation:
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GE Rui-quan. Occurrence and Geological Significance of Glauconite in Cenozoic Group of Jiyang Depression[J]. Acta Sedimentologica Sinica, 2004, 22(2): 276-280.
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Occurrence and Geological Significance of Glauconite in Cenozoic Group of Jiyang Depression
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Research and Interpretation Centerof Geology Company, Shengli Petroleum Administration,SINOPEC, Dongying Shandong 257200
- Received Date: 2003-02-26
- Rev Recd Date:
2003-07-11
- Publish Date:
2004-06-10
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Abstract
It is indicated that glauconites have been found in Cenozoic group strata in Zhan-che sag of Jiyang depression by a variety of thin section identification, and which are all in the primary state. Though deposited in different epochs, they are relatively concentrated in the study area, that is, mostly ccurred inthe strata of Cenozoic Paleogene from No.1 to No.4 of Shahejie Formation. Based on the analysis of biology fossils, it is considered that Zhan-che sag of Jiyang depression was ever invaded by the small-scalemarinetransgression under the background of the continental basin, which influenced sedimentary environment at that time, and occurred biologic variation and glauconite deposit to a certain extent. It is helpful to confirm the sedimentary environment by analyzing glauconite formation.
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References
[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] |
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Proportional views
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