济阳坳陷新生界海绿石的存在及其地质意义

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济阳坳陷新生界海绿石的存在及其地质意义

文章导航 > 沉积学报 > 2004 > 22(2): 276-280

葛瑞全. 济阳坳陷新生界海绿石的存在及其地质意义[J]. 沉积学报, 2004, 22(2): 276-280.

引用本文:

葛瑞全. 济阳坳陷新生界海绿石的存在及其地质意义[J]. 沉积学报, 2004, 22(2): 276-280.

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.

葛瑞全. 济阳坳陷新生界海绿石的存在及其地质意义[J]. 沉积学报, 2004, 22(2): 276-280.

引用本文:

葛瑞全. 济阳坳陷新生界海绿石的存在及其地质意义[J]. 沉积学报, 2004, 22(2): 276-280.

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.

济阳坳陷新生界海绿石的存在及其地质意义

葛瑞全

胜利石油管理局地质录井公司研究解释中心山东东营 257200

作者简介:
葛瑞全,男 1967年出生,石油地质

中图分类号: P512.2

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文章访问数: 584
HTML全文浏览量: 7
PDF下载量: 445
被引次数: 0

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

GE Rui-quan

Research and Interpretation Centerof Geology Company, Shengli Petroleum Administration,SINOPEC, Dongying Shandong 257200

摘要: 大量的薄片鉴定资料表明,济阳坳陷沾车凹陷新生界地层中含有海绿石矿物,并且均为原生海绿石。尽管其沉积时代不同,但分布范围相对集中,即主要分布于古近系沙四段上部沙一段的底部。结合古生物化石的分析,认为济阳坳陷沾车凹陷在陆相湖盆沉积的大背景下,曾遭受过小规模的海侵,对当时的沉积环境产生了一定影响,由此在一定程度上产生了生物的变异和海绿石的沉积。对海绿石的成因分析将有助于确定当时的沉积环境。
- 沾车凹陷 /
- 古近系 /
- 海绿石 /
- 海侵
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.
- Zhan -che sag /
- paleogene /
- glauconite /
- transgression

参考文献(9)

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计量

文章访问数: 584
HTML全文浏览量: 7
PDF下载量: 445
被引次数: 0

济阳坳陷新生界海绿石的存在及其地质意义

葛瑞全

胜利石油管理局地质录井公司研究解释中心山东东营 257200

作者简介:
葛瑞全,男 1967年出生,石油地质

收稿日期: 2003-02-26
修回日期: 2003-07-11
刊出日期: 2004-06-10

中图分类号: P512.2

关键词:

摘要: 大量的薄片鉴定资料表明,济阳坳陷沾车凹陷新生界地层中含有海绿石矿物,并且均为原生海绿石。尽管其沉积时代不同,但分布范围相对集中,即主要分布于古近系沙四段上部沙一段的底部。结合古生物化石的分析,认为济阳坳陷沾车凹陷在陆相湖盆沉积的大背景下,曾遭受过小规模的海侵,对当时的沉积环境产生了一定影响,由此在一定程度上产生了生物的变异和海绿石的沉积。对海绿石的成因分析将有助于确定当时的沉积环境。

English Abstract

葛瑞全. 济阳坳陷新生界海绿石的存在及其地质意义[J]. 沉积学报, 2004, 22(2): 276-280.

引用本文:

葛瑞全. 济阳坳陷新生界海绿石的存在及其地质意义[J]. 沉积学报, 2004, 22(2): 276-280.

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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