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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.
Citation: GE Rui-quan. Occurrence and Geological Significance of Glauconite in Cenozoic Group of Jiyang Depression[J]. Acta Sedimentologica Sinica, 2004, 22(2): 276-280.

Occurrence and Geological Significance of Glauconite in Cenozoic Group of Jiyang Depression

  • Received Date: 2003-02-26
  • Rev Recd Date: 2003-07-11
  • Publish Date: 2004-06-10
  • 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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    [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]
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    [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]
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  • Received:  2003-02-26
  • Revised:  2003-07-11
  • Published:  2004-06-10

Occurrence and Geological Significance of Glauconite in Cenozoic Group of Jiyang Depression

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.

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: 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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