Geochemical characteristics of shale gas and its response to thermal maturity (Ro) in the Longmaxi formation, Dingshan area, Southeast Sichuan

被引:6
|
作者
Zhong, Cheng [1 ,2 ]
Qin, Qirong [1 ,2 ]
Fan, Cunhui [1 ,2 ]
Hu, Dongfeng [3 ]
机构
[1] Southwest Petr Univ, State Key Lab Oil & Gas Reservoir Geol & Exploita, Chengdu 610500, Sichuan, Peoples R China
[2] Southwest Petr Univ, Sch Sci & Technol, Chengdu, Sichuan, Peoples R China
[3] SINOPEC, Explorat Co, Chengdu, Sichuan, Peoples R China
关键词
longmaxi formation shale; geochemical characteristics of shale gas; methane; wetness; oil - formed gas; carbon isotope; thermal maturity; MISSISSIPPIAN BARNETT; MARINE; CARBON; BASIN; FRACTIONATION; REVERSALS; TEXAS;
D O I
10.1080/10916466.2018.1558241
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
The composition and carbon isotope distribution of shale gas from the Longmaxi Formation in the Dingshan area were measured, and their responses to thermal maturity (Ro) were analyzed. The results show that the shale gas is mainly composed of methane (97.98-98.99%), ethane, propane and nonhydrocarbon gases (N-2 and CO2) and is an organic high temperature oil-type cracked gas. The wetness value [(C-2+C-3)/(C-1+C-2+C-3) x 100%] ranges from 0.39% to 0.74%. The early (Ro > 1.3%) residual kerogen and crude oil cracking gas was mixed with the late (Ro > 2.0%) secondary cracking gas, resulting in the full inversion of the carbon isotope sequence (C-13(1)>C-13(2)>C-13(3)).
引用
收藏
页码:1270 / 1278
页数:9
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