Role of overlying and underlying limestones in the natural hydraulic fracturing of shale sections: The case of marine–continental transitional facies in the Southern North China Basin

A few limestone layers usually underlie and/or overlie the shale layers/sections in marine facies, especially in marine–continental transitional facies (MCTF). The role of limestones in the natural hydraulic fracturing of shale sections will help in selecting the fracturing location, improving the s...

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Autores principales: Zhipeng Huo, Jianbo Gao, Jinchuan Zhang, Dong Zhang, Yutao Liang
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Lenguaje:EN
Publicado: Elsevier 2021
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Acceso en línea:https://doaj.org/article/66ccaa7b963c463d837b86ef4b6185c8
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spelling oai:doaj.org-article:66ccaa7b963c463d837b86ef4b6185c82021-11-28T04:34:25ZRole of overlying and underlying limestones in the natural hydraulic fracturing of shale sections: The case of marine–continental transitional facies in the Southern North China Basin2352-484710.1016/j.egyr.2021.11.025https://doaj.org/article/66ccaa7b963c463d837b86ef4b6185c82021-11-01T00:00:00Zhttp://www.sciencedirect.com/science/article/pii/S2352484721011628https://doaj.org/toc/2352-4847A few limestone layers usually underlie and/or overlie the shale layers/sections in marine facies, especially in marine–continental transitional facies (MCTF). The role of limestones in the natural hydraulic fracturing of shale sections will help in selecting the fracturing location, improving the stimulation power, and clarifying fracture propagation law to product more shale oil and gas. Taking an MCTF in the Southern North China Basin as an example, the differences in natural fractures and mechanical properties between limestones and shales were compared to examine the role of limestone in hydraulic fracturing. Our analyses show that shales developed more non-tectonic fractures than limestones, usually interconnected with tectonic fractures to form a fracture network. Limestones generally have a higher Young’s modulus, compressive strength, in situ stress, and fracturing pressure and a more difficult fracture initiation than shales and sandstones. Overlying and underlying limestones with less fractures and higher mechanical properties can act as an effective barrier bed, which prevents induced fractures originating from the shale sections from penetrating their mechanical interfaces into the adjacent limestone sections. This action maintains a high stimulation power in the shale sections to form a complicated induced fracture network.Zhipeng HuoJianbo GaoJinchuan ZhangDong ZhangYutao LiangElsevierarticleLimestoneShale sectionNatural fractureMechanical parameterFracturing barrierSouthern North China BasinElectrical engineering. Electronics. Nuclear engineeringTK1-9971ENEnergy Reports, Vol 7, Iss , Pp 8711-8729 (2021)
institution DOAJ
collection DOAJ
language EN
topic Limestone
Shale section
Natural fracture
Mechanical parameter
Fracturing barrier
Southern North China Basin
Electrical engineering. Electronics. Nuclear engineering
TK1-9971
spellingShingle Limestone
Shale section
Natural fracture
Mechanical parameter
Fracturing barrier
Southern North China Basin
Electrical engineering. Electronics. Nuclear engineering
TK1-9971
Zhipeng Huo
Jianbo Gao
Jinchuan Zhang
Dong Zhang
Yutao Liang
Role of overlying and underlying limestones in the natural hydraulic fracturing of shale sections: The case of marine–continental transitional facies in the Southern North China Basin
description A few limestone layers usually underlie and/or overlie the shale layers/sections in marine facies, especially in marine–continental transitional facies (MCTF). The role of limestones in the natural hydraulic fracturing of shale sections will help in selecting the fracturing location, improving the stimulation power, and clarifying fracture propagation law to product more shale oil and gas. Taking an MCTF in the Southern North China Basin as an example, the differences in natural fractures and mechanical properties between limestones and shales were compared to examine the role of limestone in hydraulic fracturing. Our analyses show that shales developed more non-tectonic fractures than limestones, usually interconnected with tectonic fractures to form a fracture network. Limestones generally have a higher Young’s modulus, compressive strength, in situ stress, and fracturing pressure and a more difficult fracture initiation than shales and sandstones. Overlying and underlying limestones with less fractures and higher mechanical properties can act as an effective barrier bed, which prevents induced fractures originating from the shale sections from penetrating their mechanical interfaces into the adjacent limestone sections. This action maintains a high stimulation power in the shale sections to form a complicated induced fracture network.
format article
author Zhipeng Huo
Jianbo Gao
Jinchuan Zhang
Dong Zhang
Yutao Liang
author_facet Zhipeng Huo
Jianbo Gao
Jinchuan Zhang
Dong Zhang
Yutao Liang
author_sort Zhipeng Huo
title Role of overlying and underlying limestones in the natural hydraulic fracturing of shale sections: The case of marine–continental transitional facies in the Southern North China Basin
title_short Role of overlying and underlying limestones in the natural hydraulic fracturing of shale sections: The case of marine–continental transitional facies in the Southern North China Basin
title_full Role of overlying and underlying limestones in the natural hydraulic fracturing of shale sections: The case of marine–continental transitional facies in the Southern North China Basin
title_fullStr Role of overlying and underlying limestones in the natural hydraulic fracturing of shale sections: The case of marine–continental transitional facies in the Southern North China Basin
title_full_unstemmed Role of overlying and underlying limestones in the natural hydraulic fracturing of shale sections: The case of marine–continental transitional facies in the Southern North China Basin
title_sort role of overlying and underlying limestones in the natural hydraulic fracturing of shale sections: the case of marine–continental transitional facies in the southern north china basin
publisher Elsevier
publishDate 2021
url https://doaj.org/article/66ccaa7b963c463d837b86ef4b6185c8
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