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Insights into Pore Structure and Fractal Characteristics of the Lower Cambrian Niutitang Formation Shale on the Yangtze Platform,South China

Insights into Pore Structure and Fractal Characteristics of the Lower Cambrian Niutitang Formation Shale on the Yangtze Platform,South China

作     者:Zixuan Liu Detian Yan Xing Niu Zixuan Liu;Detian Yan;Xing Niu

作者机构:Key Laboratory of Tectonics and Petroleum ResourcesMinistry of EducationChina University of GeosciencesWuhan 430074China School of Earth ResourcesChina University of GeosciencesWuhan 430074China Sedimentary Basin Research CenterYangtze UniversityWuhan 430074China 

出 版 物:《Journal of Earth Science》 (地球科学学刊(英文版))

年 卷 期:2020年第31卷第1期

页      面:169-180页

核心收录:

学科分类:081803[工学-地质工程] 08[工学] 0708[理学-地球物理学] 0818[工学-地质资源与地质工程] 0704[理学-天文学] 

基  金:supported by the National Natural Science Foundation of China(Nos41690131,41572327,41273001) the Program of Introducing Talents of Discipline to Universities(No.B14031) 

主  题:Niutitang Formation Yangtze area shale pore structure fractal features 

摘      要:Shales from the Lower Cambrian Niutitang Formation of Yangtze Platform have been widely investigated due to its shale gas *** better illustrate the pore structure and fractal characteristics of shale,a series of experiments were conducted on outcrop samples from the Lower Cambrian Niutitang Formation on Yangtze Platform,including X-ray diffraction(XRD),field-emission scanning electron microscopy(FE-SEM) and low-temperature nitrogen ***-Halsey-Hill(FHH) model was adopted to calculate the fractal ***,the relationships between fractal dimensions and pore structure parameters and mineral composition are ***-SEM observation results show that interparticle pores are most developed in shale,followed by intraparticle *** study identified the fractal dimensions D1(ranging from 2.558 0 to 2.710 2) and D2(ranging from 2.541 5 to 2.765 2).The pore structure of the Niutitang Formation shale is primarily controlled by quartz and clay *** dimensions are able to characterize the pore structure complexity of Niutitang Formation shale because D1 and D2 correlate well with average pore diameter and quartz content.

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