Results 191 to 200 of about 4,930 (232)
Spatiotemporal evolution analysis of multiscale fracture dynamics in hydraulic shale stimulation via integrated acoustic emission and CT imaging. [PDF]
Sci RepWei X, Cai M, Kong C, Zhao D.
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Mechanics Differences of Laminations and Crack Propagation Mechanism of Continental Shale
The International Conference on Computational & Experimental Engineering and Sciencesopenaire +1 more source
Genesis of Morphologically Distinct Quartz in Shale and Implications for Reservoir Pore and Fracture Systems: A Review. [PDF]
ACS OmegaShi M +5 more
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Surface Properties of Organic Kerogen in Continental and Marine Shale
Langmuir, 2018 The adhesion energy of kerogen in continental and marine shale was innovatively discovered using the colloid probe technique with atomic-force microscopy (AFM). AFM results indicated that the adhesion force of kerogen was higher than the inorganic material in both the continental and marine shale samples.
Shouceng Tian +11 more
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A new method for continental shale oil enrichment evaluation
Interpretation, 2017 We have evaluated continental shale oil enrichment via experiments. Rock pyrolysis, nuclear magnetic resonance, and pulse permeability tests were conducted to establish the pore saturation index (PSI), which comprehensively evaluates the enrichment of shale oil features using the characteristics of self-generation and self-preservation, the parameters
Siyuan Su +6 more
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Study on pore structure characteristics of marine and continental shale in China
Journal of Natural Gas Science and Engineering, 2016Abstract Shale gas is a key natural gas resource and has been a certain success in China. The Weiyuan marine shale (1#), Jiaoshiba marine shale (2#), Yaoqu tuff (4#) and Yaoqu continental shale (5# and 6#) were selected and subjected to thin section analyses, ice field emission scanning electron microscope (FE-SEM), mercury intrusion capillary ...
Zhiqing Li, Runqiu Huang, Tingting Du
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International Journal of Coal Geology, 2014
Abstract Continental shales in China are generally characterised by low thermal maturity and high clay content, characteristics that are significantly different from those of marine shales documented in the USA and elsewhere. Whether such continental shales have commercial hydrocarbon potential as marine shale in the USA is a question for the China ...
Xuan Tang +2 more
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Abstract Continental shales in China are generally characterised by low thermal maturity and high clay content, characteristics that are significantly different from those of marine shales documented in the USA and elsewhere. Whether such continental shales have commercial hydrocarbon potential as marine shale in the USA is a question for the China ...
Xuan Tang +2 more
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Marine and Petroleum Geology, 2019
Abstract Pore characteristics have a significant influence on the occurrence and enrichment of shale gas. Therefore, these characteristics are key parameters in shale reservoir evaluation and have important research significance. Taking a continental shale sample from the Ordos Basin, China as an example, this research used low-pressure CO2/N2 ...
Feiteng Wang, Shaobin Guo
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Abstract Pore characteristics have a significant influence on the occurrence and enrichment of shale gas. Therefore, these characteristics are key parameters in shale reservoir evaluation and have important research significance. Taking a continental shale sample from the Ordos Basin, China as an example, this research used low-pressure CO2/N2 ...
Feiteng Wang, Shaobin Guo
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Main controlling factors and movability evaluation of continental shale oil
Earth-Science Reviews, 2023Guoyong Liu, Tianwu Xu
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Injection in Shale: Experience on the Norwegian Continental Shelf
Journal of Petroleum Technology, 2016This article, written by JPT Technology Editor Chris Carpenter, contains highlights of paper SPE 170851, “Injection in Shale: Review of 15 Years of Experience on the Norwegian Continental Shelf and Implications for the Stimulation of Unconventional Reservoirs,” by F.J. Santarelli and F. Sanfilippo, Geomec, and R.W. James, H.H. Nielsen, M. Fidan, and G.
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