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| Content Provider | Springer Nature Link |
|---|---|
| Author | Jia, Chengzao Zhou, Xinyuan Wang, Zhaoming Li, Qiming Pi, Xuejun Cai, Zhenzhong Hu, Xiaoyong |
| Copyright Year | 2002 |
| Abstract | The Kela-2 gas field is located in the center of Kelasu structural belt in Kuqa Depression. This trap is one of a series of traps in the folded belts which are distributed in a string of pearls in the dual structure. The primary gas-bearing layers are sandstone of Lower Cretaceous K$_{1}$bs while the secondary layers are dolomite member and glutenite member of Lower Tertiary E$_{1–2}$km and sandstone of Lower Cretaceous K$_{1}$b. The main component of natural gas is methane whose content is higher than 97%. It is characterized by dry gas whose source rock is Jurassic coal measure. The Kela-2 structural trap was formed during the Xiyu period and then became a reservoir in the late time. The reservoir formed late and the thick seal rock of Lower Tertiary gipsmantle are the avail reason why the giant Kela-2 gas field has been well kept. The abnormal high pressure of the Kela-2 gas field results from the strong structural compression in the northern part during the Xiyu period. |
| Starting Page | 94 |
| Ending Page | 99 |
| Page Count | 6 |
| File Format | |
| ISSN | 10016538 |
| Journal | Chinese Science Bulletin |
| Volume Number | 47 |
| Issue Number | 1 |
| e-ISSN | 18619541 |
| Language | English |
| Publisher | Science in China Press |
| Publisher Date | 2002-01-01 |
| Publisher Place | Beijing |
| Access Restriction | Subscribed |
| Subject Keyword | Tarim Basin foreland basin thrust fold belt Kela-2 gas field abnormal high pressure Life Sciences Physics Chemistry/Food Science Science Geosciences Engineering |
| Content Type | Text |
| Resource Type | Article |
| Subject | Multidisciplinary |
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