Jump to content
 







Main menu
   


Navigation  



Main page
Contents
Current events
Random article
About Wikipedia
Contact us
Donate
 




Contribute  



Help
Learn to edit
Community portal
Recent changes
Upload file
 








Search  

































Create account

Log in
 









Create account
 Log in
 




Pages for logged out editors learn more  



Contributions
Talk
 



















Contents

   



(Top)
 


1 References  














Tahe oil field






Русский
 

Edit links
 









Article
Talk
 

















Read
Edit
View history
 








Tools
   


Actions  



Read
Edit
View history
 




General  



What links here
Related changes
Upload file
Special pages
Permanent link
Page information
Cite this page
Get shortened URL
Download QR code
Wikidata item
 




Print/export  



Download as PDF
Printable version
 
















Appearance
   

 






From Wikipedia, the free encyclopedia
 


Tahe
CountryChina
RegionXinjiang
Offshore/onshoreonshore
OperatorChina National Petroleum Corporation
Field history
Discovery1990
Start of production1990
Production
Estimated oil in place600 million tonnes
(~ 677×10^6 m3 or 4260 million bbl)

The Tahe oil field (Chinese: 塔河油田) is an oil field located in Xinjiang. It was discovered in 1990 and developed by China National Petroleum Corporation. It began production in 1990 and produces oil. The total proven reserves of the Tahe oil field are around 4.26 billion barrels (600×106tonnes), and production is centered on 100,000 barrels per day (16,000 m3/d).[1]

The Tahe oil field is a part of the Akekule Arch which is located in the North Uplift of the Tarim Basin. This area experienced two events of karstification which affected the Ordovician strata. The paleokarst reservoirs constituting the Tahe oil field were mostly formed by the younger, early Hercynian karstification. The oil field contains multiple caves filled with sediments, collapse breccias, and chemical fills. Sediments and collapsed breccias are characteristic for the reservoir run-off zone, whereas vadose zone is characterized by high-angle fractures and epikarst zone is characterized by weathering residues and dissolution fractures. The paleogeomorphological results indicate that paleokarst structures formed mostly in highlands and slopes during the Hercynian karstification event.[2]

References[edit]

  1. ^ "Chinese giant oilfields" (PDF). diva-portal.org. 2007. Retrieved 2014-05-11.
  • ^ Tian, Fei; Lu, Xinbian; Zheng, Songqing; Zhang, Hongfang; Rong, Yuanshuai; Yang, Debin; Liu, Naigui (2017-06-26). "Structure and Filling Characteristics of Paleokarst Reservoirs in the Northern Tarim Basin, Revealed by Outcrop, Core and Borehole Images". Open Geosciences. 9 (1): 266–280. doi:10.1515/geo-2017-0022. ISSN 2391-5447.

  • t
  • e
  • t
  • e

  • Retrieved from "https://en.wikipedia.org/w/index.php?title=Tahe_oil_field&oldid=1178311370"

    Categories: 
    Oil fields in China
    Oil field stubs
    People's Republic of China geography stubs
    Hidden categories: 
    Articles containing Chinese-language text
    China articles missing geocoordinate data
    All articles needing coordinates
    Articles missing coordinates with coordinates on Wikidata
    All stub articles
     



    This page was last edited on 2 October 2023, at 21:20 (UTC).

    Text is available under the Creative Commons Attribution-ShareAlike License 4.0; additional terms may apply. By using this site, you agree to the Terms of Use and Privacy Policy. Wikipedia® is a registered trademark of the Wikimedia Foundation, Inc., a non-profit organization.



    Privacy policy

    About Wikipedia

    Disclaimers

    Contact Wikipedia

    Code of Conduct

    Developers

    Statistics

    Cookie statement

    Mobile view



    Wikimedia Foundation
    Powered by MediaWiki