SEDIMENTARY MICROFACIES OF <i>Ed</i><sub>3</sub> IN DAWANGZHUANG AREA OF RAOYANG SAG

ZHANG Qiang; GUO Fa-jun; XIE Jun; ZHANG Shu-juan; CHEN Xiao-qin; HAO Peng; XU Min

2020 Vol. 29, No. 3

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Article navigation > Geology and Resources > 2020 > 29(3): 252-259

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ZHANG Qiang, GUO Fa-jun, XIE Jun, ZHANG Shu-juan, CHEN Xiao-qin, HAO Peng, XU Min. SEDIMENTARY MICROFACIES OF Ed3 IN DAWANGZHUANG AREA OF RAOYANG SAG[J]. Geology and Resources, 2020, 29(3): 252-259.

Citation:

ZHANG Qiang, GUO Fa-jun, XIE Jun, ZHANG Shu-juan, CHEN Xiao-qin, HAO Peng, XU Min. SEDIMENTARY MICROFACIES OF Ed₃ IN DAWANGZHUANG AREA OF RAOYANG SAG[J]. Geology and Resources, 2020, 29(3): 252-259.

SEDIMENTARY MICROFACIES OF Ed₃ IN DAWANGZHUANG AREA OF RAOYANG SAG

1.
School of Earth Sciences and Engineering, Shandong University of Science and Technology, Qingdao 266590, Shandong Province, China
2.
Exploration and Development Institute of Huabei Oilfield Branch, PetroChina, Renqiu 062552, Hebei Province, China
3.
Geological Institute of Erenhot Branch, Huabei Oilfield Company, Xilinhot 026000, Inner Mongolia, China

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Corresponding author: GUO Fa-jun, 15949740143@163.com

Received Date: 06 December 2019

Revised Date: 11 March 2020

Publish Date: 28 June 2020

Abstract

Abstract

To solve the problem of inconsistencies in the determination of sedimentary facies types in Dawangzhuang area, on the basis of regional tectonic evolution, with drilling data, sedimentary structure marks and logging data, this paper discusses the controlling of surrounding buried hills and subsags on the source direction and sedimentary facies types during the sedimentary period of the third member of Dongying Formation (Ed₃), and establishes the sedimentary model of Ed₃. The results show that the subsidence center is located in the northeast of study area during the sedimentary period of Ed₃, which mainly receives the provenance deposits of Shenze low salient in the southwest. During the sedimentation of Dongying Formation, with the uplifting of fault depression, the lake basin shrinks rapidly, the terrain becomes flat gradually, the sedimentary facies continues to extend, and the meandering river facies is developed in the Ed₃ of Dawangzhuang area. The detailed study of sedimentary facies provides a basis for reservoir prediction.
- Raoyang Sag /
- Paleogene /
- Dongying Formation /
- meandering river /
- Dawangzhuang area /
- Hebei Province

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References

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