scholarly journals Hydrogen isotope of natural gas from the Xujiahe Formation and its implications for water salinization in central Sichuan Basin, China

2019 ◽  
Vol 4 (4) ◽  
pp. 215-230
Author(s):  
Yunyan Ni ◽  
Fengrong Liao ◽  
Limiao Yao ◽  
Jinliang Gao ◽  
Dijia Zhang
2018 ◽  
Vol 167 ◽  
pp. 890-899 ◽  
Author(s):  
Kaiming Su ◽  
Jungang Lu ◽  
Guangwu Zhang ◽  
Shijia Chen ◽  
Yong Li ◽  
...  

2010 ◽  
Vol 37 (2) ◽  
pp. 146-157 ◽  
Author(s):  
Zhao Wenzhi ◽  
Wang Hongjun ◽  
Xu Chunchun ◽  
Bian Congsheng ◽  
Wang Zecheng ◽  
...  

2013 ◽  
Author(s):  
Xi Liao ◽  
Anthony Cortis ◽  
Long Xu ◽  
Alan Rolph ◽  
Kwong Tak Ha ◽  
...  

2013 ◽  
Author(s):  
Xi Liao ◽  
Anthony Cortis ◽  
Long Xu ◽  
Alan Rolph ◽  
Kwong Tak Ha ◽  
...  

2011 ◽  
Vol 347-353 ◽  
pp. 1701-1706
Author(s):  
Sheng Bin Zhang ◽  
Zhen Liu ◽  
Hong Jun Liu ◽  
Ya Hui Song ◽  
Xin Min Li ◽  
...  

Alkali diagenesis has been discovered firstly in Xujiahe formation in Sichuan basin. Alkali diagenesis is characterized by quartz dissolution pore. Based on thin section identification, scanning electron microscope and X-ray diffraction analysis, and considering the geological background, the characteristics and formation mechanism of alkali diagenesis in Xujiahe formation are studied thoroughly. The results indicate that the sandstone reservoir in Xujiahe formation has experienced a strong diagenesis and entered the stage of late diagenetic B. Diagenetic environment experienced a transition from acidity to alkalinity. Secondary pores produced by quartz dissolution contribute for the better quality of Xu_2 reservoir.


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