Pore structure characterization for the Longmaxi and Niutitang shales in the Upper Yangtze Platform, South China: Evidence from focused ion beam He ion microscopy, nano-computerized tomography and gas adsorption analysis

被引:132
作者
Wang, Pengfei [1 ,2 ]
Jiang, Zhenxue [1 ,2 ]
Chen, Lei [1 ,2 ]
Yin, Lishi [1 ,2 ]
Li, Zhuo [1 ,2 ]
Zhang, Chen [1 ,2 ]
Tang, Xianglu [1 ,2 ]
Wang, Guozhen [1 ,2 ]
机构
[1] China Univ Petr, State Key Lab Petr Resources & Prospecting, Beijing 102249, Peoples R China
[2] China Univ Petr, Unconvent Nat Gas Res Inst, Beijing 102249, Peoples R China
基金
中国国家自然科学基金;
关键词
Upper Yangtze platform; Longmaxi shale; Niutitang shale; Pore structure; Thermal maturity; ORGANIC-RICH SHALES; HIGH THERMAL MATURITY; SICHUAN BASIN; LACUSTRINE SHALE; FRACTAL CHARACTERISTICS; SPACE MORPHOLOGY; PERMIAN SHALES; SONGLIAO BASIN; BARNETT SHALE; SURFACE-AREA;
D O I
10.1016/j.marpetgeo.2016.09.001
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Pore structure is of great importance in the occurrence of shale gas. In this study, pores in shale samples from the Lower Silurian Longmaxi and Lower Cambrian Niutitang shales in Chongqing, in the Upper Yangtze Platform, South China, were examined using focused ion beam-He ion microscopy (FIB-HIM), nano-computerized tomography (nano-CT), and gas adsorption analysis. The results show that most pores in measured samples of the Niutitarig shale are mineral matrix pores and have poor connectivity, including both intraparticle and interparticle pores. Organic matter pores in measured samples of the Niutitang shale are rare and have small diameters. In measured samples of the Longmaxi shale, OM pores-mostly macropores and large mesopores-are the most abundant. The nano-CT results revealed that the abundance of OM pores led to good pore connectivity in the Longmaxi shale samples, whereas the prevalence of mineral matrix pores resulted in poor connectivity in the Niutitang shale samples. N-2 and CO2 adsorption analyses showed that the mean value of micropore-mesopore volumes in the Niutitang and Longmaxi shales samples are 0.0332 ml/g and 0.0261 ml/g, respectively. The mean values of micropores-mesopores surface area in the Niutitang and Longmaxi shales samples are 33.84 m(2)/g and 32.46 m(2)/g, respectively. Thus, there is little difference between measured samples of the Longmaxi and Niutitang shales in terms of volume and surface area of micropores-mesopores. The equal-vitrinite reflectance (equal-Ro) values of measured samples of the Longmaxi shale are lower than those of the Niutitang shale samples. Over-maturity (equal-Ro>3%) resulted in a reduction of the number of pores in organic matter, small pore size, and poor connectivity in measured samples of the Niutitang shale. Relatively low maturity (2%<equal-Ro<3%) resulted in better preservation of OM pores and good connectivity in measured samples of the Longmaxi shale. It is concluded that suitable thermal maturity is beneficial for pore development in shale, which is of great significance for shale gas exploration and development. (C) 2016 Elsevier Ltd. All rights reserved.
引用
收藏
页码:1323 / 1337
页数:15
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