Analysis of the Formation Mechanism of Upper Paleozoic Clastic Rock Reservoir in the Southeastern Ordos Basin

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Authors

  • Chengdu university of Technology, Chengdu, Sichuan, 610059 ,CN

Keywords:

Upper Paleozoic, Clastic Reservoir, Formation Mechanism, Ordos Basin.

Abstract

The formation mechanism of clastic reservoirs in the Upper paleozoic in southeastern Ordos basin is systematically studied by using a large number of rock and mineral analysis and testing data. It is pointed out that the sedimentary environment, petrological characteristics, burial diagenesis, abnormally high fluid pressure and medium environment of salt lake water are the formation mechanisms that control the diagenetic evolution and reservoir property of the reservoirs. And it is put forward that the main reservoir space for the high efficiency reservoirs of sandstone in the upper paleozoic of the Ordos basin includes various types of denudation pores and residual intergranular pores, and that the plastic particle content and particle size in the detrital component of the reservoir are the important mechanisms for the formation of the reservoir.

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Published

2022-10-23

How to Cite

Yan, L. (2022). Analysis of the Formation Mechanism of Upper Paleozoic Clastic Rock Reservoir in the Southeastern Ordos Basin. Journal of Mines, Metals and Fuels, 66(9), 531–536. Retrieved from https://www.informaticsjournals.com/index.php/jmmf/article/view/31755

 

References

Shuai Y, Zhang S, Mi J, Gong S Yuan, X, Yang Z. (2013): “Charging time of tight gas in the upper paleozoic of the Ordos basin, central China”, Organic Geochemistry, 64(6), 38-46.

Xu H, Tang D, Zhang J, Yin W, Zhang W, Lin W. (2011): “Factors affecting the development of the pressure differential in upper paleozoic gas reservoirs in the sulige and yulin areas of the Ordos basin, China”, International Journal of Coal Geology, 85(1), 103-111.

Kuznetsov nB, Soboleva aa, Miller EL, udoratina OV, Gehrel G, Romanyuk TV. (2013): “First u-pb datings of detrital zircons from middle and upper paleozoic sandstones of the polar urals: testing the regional tectonic models”, Doklady Earth Sciences, 451(1), 692-697.

Mora-Gutiérrez Ra, Rincón-García Ea, Ponsich a, Ramírez-Rodríguez J, Méndez-Gurrola II. (2016): “Influence of social network on method musical composition”, Artificial Intelligence Review, 46(2), 225-266.

Lucas SG. (2013): “Vertebrate biostratigraphy and biochronology of the upper paleozoic dunkard group, Pennsylvania-West Virginia–Ohio, uSa”, International Journal of Coal Geology, 119(119), 79-87.

Mi J, He K, Tao S, Yang C, Sun M. (2016): “Geochemical comparison between the gas in bulk fluid inclusions and reservoir gas produced in paleozoic formation, Ordos basin, China”, Journal of Geochemical Exploration, 171, 133-140.

Qiu n, Chang J, Zuo Y, Wang J, Li H. (2012): “Thermal evolution and maturation of lower paleozoic source rocks in the Tarim basin, northwest China”, Aapg Bulletin, 96(96), 789-821.

Zhao X, Liu C, Wan J, Zhao Y, Wang L, Zhang Q. (2016): “Detrital zircon u-pb ages of paleozoic sedimentary rocks from the eastern hexi corridor belt (nW China): provenance and geodynamic implications”, Sedimentary Geology, 339, 32-45.