沾化凹陷东部长堤地区下第三系沉积体系研究

国景星; 戴启德; 徐炜

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沾化凹陷东部长堤地区下第三系沉积体系研究

国景星, 戴启德, 徐炜

文章导航 > 沉积学报 > 2001 > 19(3): 368-374

国景星, 戴启德, 徐炜. 沾化凹陷东部长堤地区下第三系沉积体系研究[J]. 沉积学报, 2001, 19(3): 368-374.

引用本文:

国景星, 戴启德, 徐炜. 沾化凹陷东部长堤地区下第三系沉积体系研究[J]. 沉积学报, 2001, 19(3): 368-374.

GUO Jing xing, DAI Qi de, XU Wei. Study on the Sedimentary System of Paleogene in Changdi Region of Zhanhua Sag[J]. Acta Sedimentologica Sinica, 2001, 19(3): 368-374.

Citation:

GUO Jing xing, DAI Qi de, XU Wei. Study on the Sedimentary System of Paleogene in Changdi Region of Zhanhua Sag[J]. Acta Sedimentologica Sinica, 2001, 19(3): 368-374.

国景星, 戴启德, 徐炜. 沾化凹陷东部长堤地区下第三系沉积体系研究[J]. 沉积学报, 2001, 19(3): 368-374.

引用本文:

国景星, 戴启德, 徐炜. 沾化凹陷东部长堤地区下第三系沉积体系研究[J]. 沉积学报, 2001, 19(3): 368-374.

GUO Jing xing, DAI Qi de, XU Wei. Study on the Sedimentary System of Paleogene in Changdi Region of Zhanhua Sag[J]. Acta Sedimentologica Sinica, 2001, 19(3): 368-374.

Citation:

GUO Jing xing, DAI Qi de, XU Wei. Study on the Sedimentary System of Paleogene in Changdi Region of Zhanhua Sag[J]. Acta Sedimentologica Sinica, 2001, 19(3): 368-374.

沾化凹陷东部长堤地区下第三系沉积体系研究

1.
中国矿业大学,江苏徐州 221008;
2.
石油大学石油资源科学系,山东东营 257061

详细信息

作者简介:
国景星,男,1963年出生,副教授,油气储层地质学、石油地质学

中图分类号: te121.3

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文章访问数: 447
HTML全文浏览量: 17
PDF下载量: 704
被引次数: 0

Study on the Sedimentary System of Paleogene in Changdi Region of Zhanhua Sag

1.
China University of Mining and Technology,Xuzhou,Jiangsu 221008;
2.
Department of Petroleum Resource Sciences,University of Petroleum, Dongying,Shandong 257061

摘要

摘要: 综合运用地质、测井、地震及分析化验等资料,对沾化凹陷东部长堤地区下第三系沉积体系进行了较为全面系统的研究,认为长堤地区下第三系发育有水下扇、滨浅湖滩坝、扇三角洲、浊积和辫状河等 5类沉积体系。并阐述了各类沉积体系在本区的亚相、微相类型及其特征,系统分析了早第三纪不同阶段的沉积相类型及其分布特征,探讨了不同时期物源区及古水流流向,总结了垂向上沉积体系的演化等。
- 沾化凹陷 /
- 长堤地区 /
- 下第三系 /
- 沉积体系 /
- 沉积亚相 /
- 沉积微相
Abstract: Changdi region is situated in the eastern part of Zhanhua sag in Jiyang depression．It belongs to one part of the Zhuangxi-Gudong buried hill belt in Structure．with area an about 160 km²．Based on the synthetical analysis the geologieal,log,seismic and chemical analysis data,the authors believe 5 types of sedimentary system were developed in this area in Paleogene,that is,subsurface fan,beach and dam,fan delta,turbidity current and braided river. Subsurface fan can be divided 3 types of sub-facieses,i,e,root-fan,middle-fan and fan edge by core and conglomerate distribution and etc．the middle-fan can be divided 3 micro-facies-braided channel．space between channel and front-edge zone．In the braided channel,sediment grain is coatse．And it shows positive rhythm,SP curve with box type and atc．Surface of scour can be seen at the bottom of the channel． Beach and bar system were formed at the edge of lake．shallow platform and etc．They can be divided into 2 types,i．e．,terrigenous debris type and carbonate rock type．The terrigenous debris type was distributed mainly over the west edge of the study area．and carbonate rock type was distributed mainly in the middle part．About the fan delta system．there were prodelta and delta front in the area．The delta front subfaces consists of embranchment channel,channel mouth bar and etc．Judged by distribution of the sedimentary system,during the third member of Shahejie formation,researching area belongs to subsurface fan system．From the early stage to metaphase,the sediment range were widened gradually．In the later period,the range of lake and size of subsurface fan diminished．During the second member and the early stage of the first member of the Shahejie Formation,this area belonged to beach and bar system．In the third member of Dongying Formation,the study area belonged to fan delta system,and it stretched gradually from southeast to north．duing the later period,the southeast part developed the fan delta plain．The delta front subfaces consisted of embranchment channel,channel mouth bar and etc． During the second member and the first member of the Dongying Formation,this area belonged to braided river system as a whole．There were a series of channel bar deposits． It was thought by synthetically analyzing the regularity of vertical evolution of sedimentary system was stinct．During the third and second member of the Shahejie Formation．the type of sedimentary system was subsurface fan near bank,the sediments came from Changdi lower upheaval．During the first member of the Shahejie Formation．it belonged to beach and bar system,while later period of the member,it was deep lake．From the third member of the Dongying Formation to the second and first member。the sediment system was fan delta,braided river,sediments mostly came from the Kendong—Qingtuozi upheaval．
- Zhanhua Sag /
- Changdi region /
- Paleogene /
- sedimentary system /
- sedimentar subfacies /
- sedl&mdash

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参考文献(1)

[1]	1.《胜利油田石油地质志》编写组中国石油地质志(卷六) 1993 2.陈立官油气田地下地质学 1983 3.冯增昭沉积岩石学 1993 4.徐怀大地震地层学解释基础 1990 5.冯增昭中国沉积学 1994 6.吴崇筠中国含油气盆地沉积学 1993 7.纪友亮陆相断陷湖盆层序地层学 1996

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沾化凹陷东部长堤地区下第三系沉积体系研究

1. 中国矿业大学,江苏徐州 221008;

2. 石油大学石油资源科学系,山东东营 257061

作者简介:
国景星,男,1963年出生,副教授,油气储层地质学、石油地质学

收稿日期: 2000-07-14
修回日期: 2000-08-31
刊出日期: 2001-09-10

中图分类号: te121.3

关键词:

摘要: 综合运用地质、测井、地震及分析化验等资料,对沾化凹陷东部长堤地区下第三系沉积体系进行了较为全面系统的研究,认为长堤地区下第三系发育有水下扇、滨浅湖滩坝、扇三角洲、浊积和辫状河等 5类沉积体系。并阐述了各类沉积体系在本区的亚相、微相类型及其特征,系统分析了早第三纪不同阶段的沉积相类型及其分布特征,探讨了不同时期物源区及古水流流向,总结了垂向上沉积体系的演化等。

English Abstract

Study on the Sedimentary System of Paleogene in Changdi Region of Zhanhua Sag

1. China University of Mining and Technology,Xuzhou,Jiangsu 221008;

2. Department of Petroleum Resource Sciences,University of Petroleum, Dongying,Shandong 257061

Received Date: 2000-07-14
Rev Recd Date: 2000-08-31
Publish Date: 2001-09-10

Keywords:

Abstract: Changdi region is situated in the eastern part of Zhanhua sag in Jiyang depression．It belongs to one part of the Zhuangxi-Gudong buried hill belt in Structure．with area an about 160 km²．Based on the synthetical analysis the geologieal,log,seismic and chemical analysis data,the authors believe 5 types of sedimentary system were developed in this area in Paleogene,that is,subsurface fan,beach and dam,fan delta,turbidity current and braided river. Subsurface fan can be divided 3 types of sub-facieses,i,e,root-fan,middle-fan and fan edge by core and conglomerate distribution and etc．the middle-fan can be divided 3 micro-facies-braided channel．space between channel and front-edge zone．In the braided channel,sediment grain is coatse．And it shows positive rhythm,SP curve with box type and atc．Surface of scour can be seen at the bottom of the channel． Beach and bar system were formed at the edge of lake．shallow platform and etc．They can be divided into 2 types,i．e．,terrigenous debris type and carbonate rock type．The terrigenous debris type was distributed mainly over the west edge of the study area．and carbonate rock type was distributed mainly in the middle part．About the fan delta system．there were prodelta and delta front in the area．The delta front subfaces consists of embranchment channel,channel mouth bar and etc．Judged by distribution of the sedimentary system,during the third member of Shahejie formation,researching area belongs to subsurface fan system．From the early stage to metaphase,the sediment range were widened gradually．In the later period,the range of lake and size of subsurface fan diminished．During the second member and the early stage of the first member of the Shahejie Formation,this area belonged to beach and bar system．In the third member of Dongying Formation,the study area belonged to fan delta system,and it stretched gradually from southeast to north．duing the later period,the southeast part developed the fan delta plain．The delta front subfaces consisted of embranchment channel,channel mouth bar and etc． During the second member and the first member of the Dongying Formation,this area belonged to braided river system as a whole．There were a series of channel bar deposits． It was thought by synthetically analyzing the regularity of vertical evolution of sedimentary system was stinct．During the third and second member of the Shahejie Formation．the type of sedimentary system was subsurface fan near bank,the sediments came from Changdi lower upheaval．During the first member of the Shahejie Formation．it belonged to beach and bar system,while later period of the member,it was deep lake．From the third member of the Dongying Formation to the second and first member。the sediment system was fan delta,braided river,sediments mostly came from the Kendong—Qingtuozi upheaval．

国景星, 戴启德, 徐炜. 沾化凹陷东部长堤地区下第三系沉积体系研究[J]. 沉积学报, 2001, 19(3): 368-374.

引用本文:

国景星, 戴启德, 徐炜. 沾化凹陷东部长堤地区下第三系沉积体系研究[J]. 沉积学报, 2001, 19(3): 368-374.

GUO Jing xing, DAI Qi de, XU Wei. Study on the Sedimentary System of Paleogene in Changdi Region of Zhanhua Sag[J]. Acta Sedimentologica Sinica, 2001, 19(3): 368-374.

Citation:

GUO Jing xing, DAI Qi de, XU Wei. Study on the Sedimentary System of Paleogene in Changdi Region of Zhanhua Sag[J]. Acta Sedimentologica Sinica, 2001, 19(3): 368-374.

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沾化凹陷东部长堤地区下第三系沉积体系研究

作者简介:
国景星,男,1963年出生,副教授,油气储层地质学、石油地质学

计量

Study on the Sedimentary System of Paleogene in Changdi Region of Zhanhua Sag

计量

目录

沾化凹陷东部长堤地区下第三系沉积体系研究

1. 中国矿业大学,江苏徐州 221008;

2. 石油大学石油资源科学系,山东东营 257061

作者简介:
国景星,男,1963年出生,副教授,油气储层地质学、石油地质学

English Abstract

Study on the Sedimentary System of Paleogene in Changdi Region of Zhanhua Sag

1. China University of Mining and Technology,Xuzhou,Jiangsu 221008;

2. Department of Petroleum Resource Sciences,University of Petroleum, Dongying,Shandong 257061

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沾化凹陷东部长堤地区下第三系沉积体系研究

作者简介: 国景星,男,1963年出生,副教授,油气储层地质学、石油地质学

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Study on the Sedimentary System of Paleogene in Changdi Region of Zhanhua Sag

计量

出版历程

目录

沾化凹陷东部长堤地区下第三系沉积体系研究

1. 中国矿业大学,江苏徐州 221008; 2. 石油大学石油资源科学系,山东东营 257061

作者简介: 国景星,男,1963年出生,副教授,油气储层地质学、石油地质学

English Abstract

Study on the Sedimentary System of Paleogene in Changdi Region of Zhanhua Sag

1. China University of Mining and Technology,Xuzhou,Jiangsu 221008; 2. Department of Petroleum Resource Sciences,University of Petroleum, Dongying,Shandong 257061

全文HTML

目录

友情链接

期刊在线

联系我们

作者简介:
国景星,男,1963年出生,副教授,油气储层地质学、石油地质学

1. 中国矿业大学,江苏徐州 221008;

2. 石油大学石油资源科学系,山东东营 257061

作者简介:
国景星,男,1963年出生,副教授,油气储层地质学、石油地质学

1. China University of Mining and Technology,Xuzhou,Jiangsu 221008;

2. Department of Petroleum Resource Sciences,University of Petroleum, Dongying,Shandong 257061