Geochemical characteristics and origin of natural gas and gas -filling mode of the Paleozoic in the Yanchuannan gas field, Ordos Basin, China

2018 ◽  
Vol 49 ◽  
pp. 286-297 ◽  
Author(s):  
Shuling Tang ◽  
Dazhen Tang ◽  
Song Li ◽  
Yunguang Geng ◽  
Hao Xu ◽  
...  
2017 ◽  
Vol 46 ◽  
pp. 515-525 ◽  
Author(s):  
Ke Wang ◽  
Xiongqi Pang ◽  
Zhengfu Zhao ◽  
Shan Wang ◽  
Tao Hu ◽  
...  

2016 ◽  
Vol 102 ◽  
pp. 67-76 ◽  
Author(s):  
Ziqi Feng ◽  
Dan Liu ◽  
Shipeng Huang ◽  
Deyu Gong ◽  
Weilong Peng

2009 ◽  
Vol 35 (1) ◽  
pp. 74-88 ◽  
Author(s):  
Quanyou Liu ◽  
Mengjin Chen ◽  
Wenhui Liu ◽  
Jian Li ◽  
Pinlong Han ◽  
...  

2019 ◽  
Vol 157 (4) ◽  
pp. 527-538 ◽  
Author(s):  
Wenxue Han ◽  
Xiangchun Chang ◽  
Weijiao Ma ◽  
Shizhen Tao ◽  
Jingli Yao ◽  
...  

AbstractThe carbon isotope value of ethane in the southern part of the Jingbian gas field is lower than that in the northern part, indicating a carbon isotopic reversal in the southern Jingbian gas field (δ13Cmethane > δ13Cethane). Through comparing the geochemical characteristics of gases in the southern and northern parts of the gas field, the reasons for the carbon isotopic reversal in the southern Jingbian gas field were determined to be high thermal maturity and mixing action. When thermal maturity reaches a critical value, the carbon isotope value of ethane becomes relatively more depleted with thermal maturity. Although the carbon isotope value of methane increases with thermal maturity, the extent is relatively smaller. Finally, the rare phenomenon of δ13Cmethane > δ13Cethane occurs. High thermal maturity leads to the secondary thermal cracking of gases. Mixing of the cracked gases and primary gases also leads to carbon isotopic reversal. Both of the above mechanisms share a common premise, which is high thermal maturity.


2021 ◽  
Vol 200 ◽  
pp. 108406
Author(s):  
Kaiming Su ◽  
Shijia Chen ◽  
Yuting Hou ◽  
Haifeng Zhang ◽  
Xiaolei Zhang ◽  
...  

Sign in / Sign up

Export Citation Format

Share Document