Comment on "Formation of nanoporous pyrobitumen residues during maturation of the Barnett Shale (Fort Worth Basin)" by Bernard et al. (2012)

被引:50
作者
Reed, Robert M. [1 ]
Loucks, Robert G. [1 ]
Ruppel, Stephen C. [1 ]
机构
[1] Univ Texas Austin, Jackson Sch Geosci, Bur Econ Geol, Austin, TX 78713 USA
关键词
Pore; Mudrock; Organic matter; Maturity; SEM; BIB-SEM; MORPHOLOGY;
D O I
10.1016/j.coal.2013.11.012
中图分类号
TE [石油、天然气工业]; TK [能源与动力工程];
学科分类号
0807 ; 0820 ;
摘要
In their 2012 paper discussing the character of pores and organic matter in the Mississippian Barnett Shale, Bernard et al. (2012) identified only nonporous kerogen and nonporous solid bitumen in oil-window-maturity samples, but nanoporous pyrobitumen in gas-window-maturity samples. Our examination of samples from the same wells shows that pores are also present in organic matter from oil-window-maturity samples. We also argue that some of the pores we identified in gas-window-maturity samples are developed in organic matter that is unlikely to be pyrobitumen. (C) 2013 Elsevier B.V. All rights reserved.
引用
收藏
页码:111 / 113
页数:3
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