Structural Style in Gentle Slope and its Control Action for Sedimentary and Reservoir Formation of Chenjiazhuang Area in Jiyang Depression for Case

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Haft-graben fault basin often have large-scale gentle slope, and the zone of structural style, sedimentary types and forming factor has its unique characteristics. This paper takes Chenjiazhuang area in Jiyang depression for example. By constructing, deposition and accumulation of combining methods Chenjiazhuang area can be divided into three major tectonic units, witch are upliftt zone, slope zone and structural slope-break zone. Different tectonic units develop different sedimentary and reservoir types, and the accumulation controlling factors are also larger differences.

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84-91

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February 2011

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© 2011 Trans Tech Publications Ltd. All Rights Reserved

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[1] Wang Binhai, Qian Kai. Geologic Research and Exploration Practice in Shengli Petroleum Province. University of Petroleum Press, (1992).

Google Scholar

[2] Zhang Shanwen. A discussion on Shallow Layer Prospecting in Zhanhua sag. Composite Oil and Gas Field, 1999, Issue 3, P6~7.

Google Scholar

[3] Fei Baosheng. Hydrocarbon Exploration on gentle slope belt in dustpan-like sag. Composite Oil and Gas Field, 1999, Issue 3, P1~5.

Google Scholar

[4] XIe Taijun, Pan Zuyin and Yang Xuechang. System of Hydrocarbon Migration Agent and Pathway. Science Press. 1997: P385~405.

Google Scholar

[5] Li Chunguang. Analysis on Regional Caprocks and its control on Oil and Gas Distribution of Dongying Rift Basin. Oil & Gas Geology. 21(2): P133~135.

Google Scholar

[6] Zhang Zhaolu, Wang Hua and Yang Hong. Study on passage system of petroliferous basins. Oil & Gas Geology. 21(2): P133~135.

Google Scholar

[7] Zeng Jianhui, Wang Hongyu. An Experimental Study of Petroleum Migration and Accumulation in Carrier Bed and Lithological Ttrap. Earth Science(Journal of China University of Geosciences). 1999, 24(2): P193~196 Figure1 Zone position of Chenjiazhuang area Figure 2 Sedimentary and reservoir mode of Chenjiazhuang area Figure 3 Reservoir profile of Well Chen164 to Well Chen165 Figure 4 Reservoir profile of Well Chen164 to Well Chen165.

DOI: 10.17816/snv201761114.f41581

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