中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
首页 机构 成果 学者
  
  1. CAS IR Grid
  2. 地质与地球物理研究所
  3. 中国科学院地质与地球物理研究所
Investigation of formation and evolution of organic matter pores in marine shale by helium ion microscope: An example from the Lower Silurian Longmaxi Shale, South China

文献类型：期刊论文

作者Huang, Cheng3; Ju, Yiwen3; Zhu, Hongjian3; Lash, Gary G.2; Qi, Yu1; Yu, Kun3; Feng, Hongye3; Ju, Liting3; Qiao, Peng3
刊名MARINE AND PETROLEUM GEOLOGY
出版日期2020-10-01
卷号120页码:11
关键词OM pore Organic-rich marine shale HIM Porosity evolution South China
ISSN号0264-8172
DOI10.1016/j.marpetgeo.2020.104550
英文摘要Using a helium ion microscope (HIM), we carefully observed and analyzed organic matter (OM) pores in several Longmaxi shale samples collected from the Upper Yangtze Platform, South China. The results indicate that the formation process of OM pore essentially involves gradual expansion and connection of defects/space within OM. This process, which is divided into the four stages of formation, expansion, connection, and consolidation, can involve pore scales ranging from a few nanometers to over a micrometer under HIM. More specifically, spotted spherical pores first form within OM, then expand until they connect to adjacent pores. Within large areas of such connectivity, "pit" structures eventually form, preliminarily defined as OM pores that are significantly larger than surrounding pores, essentially being greater than 100 nm in size. As the final stage of OM pore evolution, the shape and size of "pit" structures can be limited by the framework of mineral particles around or within the OM. Additionally, we found that surrounding pores are smaller when "pit" structures develop, perhaps because removal of side chains of OM tends to occur on the inner surface of the formed pores, leading them to rapidly expand, or because OM particles have differing compositions or structures, some of which may be unfavorable to pore development.
WOS关键词UPPER YANGTZE PLATFORM ; NANOMETER-SCALE PORES ; GAS-ADSORPTION ; ALBANY SHALE ; POROSITY ; BARNETT ; DEFORMATION ; MATURATION ; PYROLYSIS ; MARCELLUS
资助项目National Natural Science Foundation of China[41530315] ; National Natural Science Foundation of China[41872160] ; National Natural Science Foundation of China[41372213] ; National Science and Technology Major Project of China[2016ZX05066003] ; National Science and Technology Major Project of China[2016ZX05066006] ; "Climate Change: Carbon Budget and Related Issues" Strategic Priority Research Program of the Chinese Academy of Sciences[XDA05030100] ; Sichuan Science and Technology Support Program[2016JZ0037]
WOS研究方向Geology
语种英语
WOS记录号WOS:000569007300002
出版者ELSEVIER SCI LTD
资助机构National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Science and Technology Major Project of China ; National Science and Technology Major Project of China ; "Climate Change: Carbon Budget and Related Issues" Strategic Priority Research Program of the Chinese Academy of Sciences ; "Climate Change: Carbon Budget and Related Issues" Strategic Priority Research Program of the Chinese Academy of Sciences ; Sichuan Science and Technology Support Program ; Sichuan Science and Technology Support Program ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Science and Technology Major Project of China ; National Science and Technology Major Project of China ; "Climate Change: Carbon Budget and Related Issues" Strategic Priority Research Program of the Chinese Academy of Sciences ; "Climate Change: Carbon Budget and Related Issues" Strategic Priority Research Program of the Chinese Academy of Sciences ; Sichuan Science and Technology Support Program ; Sichuan Science and Technology Support Program ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Science and Technology Major Project of China ; National Science and Technology Major Project of China ; "Climate Change: Carbon Budget and Related Issues" Strategic Priority Research Program of the Chinese Academy of Sciences ; "Climate Change: Carbon Budget and Related Issues" Strategic Priority Research Program of the Chinese Academy of Sciences ; Sichuan Science and Technology Support Program ; Sichuan Science and Technology Support Program ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Science and Technology Major Project of China ; National Science and Technology Major Project of China ; "Climate Change: Carbon Budget and Related Issues" Strategic Priority Research Program of the Chinese Academy of Sciences ; "Climate Change: Carbon Budget and Related Issues" Strategic Priority Research Program of the Chinese Academy of Sciences ; Sichuan Science and Technology Support Program ; Sichuan Science and Technology Support Program
源URL[http://ir.iggcas.ac.cn/handle/132A11/98239]  
专题中国科学院地质与地球物理研究所
通讯作者Ju, Yiwen
作者单位1.Chinese Acad Sci, Inst Geol & Geophys, Beijing 100049, Peoples R China
2.SUNY Coll Fredonia, Dept Geol & Environm Sci, Fredonia, NY 14063 USA
3.Chinese Acad Sci, Univ Chinese Acad Sci, Coll Earth & Planetary Sci, Key Lab Computat Geodynam, Beijing 100049, Peoples R China
推荐引用方式
GB/T 7714		 Huang, Cheng,Ju, Yiwen,Zhu, Hongjian,et al. Investigation of formation and evolution of organic matter pores in marine shale by helium ion microscope: An example from the Lower Silurian Longmaxi Shale, South China[J]. MARINE AND PETROLEUM GEOLOGY,2020,120:11.
APA Huang, Cheng.,Ju, Yiwen.,Zhu, Hongjian.,Lash, Gary G..,Qi, Yu.,...&Qiao, Peng.(2020).Investigation of formation and evolution of organic matter pores in marine shale by helium ion microscope: An example from the Lower Silurian Longmaxi Shale, South China.MARINE AND PETROLEUM GEOLOGY,120,11.
MLA Huang, Cheng,et al."Investigation of formation and evolution of organic matter pores in marine shale by helium ion microscope: An example from the Lower Silurian Longmaxi Shale, South China".MARINE AND PETROLEUM GEOLOGY 120(2020):11.

入库方式： OAI收割

来源：地质与地球物理研究所

浏览0
下载0
收藏0
其他版本

除非特别说明，本系统中所有内容都受版权保护，并保留所有权利。