松辽盆地新立地区浅水三角洲水下分流河道砂体结构解剖

王家豪; 陈红汉; 江涛; 唐振兴; 赵宝峰; 徐东浩

doi:10.3799/dqkx.2012.062

Volume 37 Issue 3

May 2012

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Article Navigation > Earth Science > 2012 > 37(3): 556-564

WANG Jia-hao, CHEN Hong-han, JIANG Tao, TANG Zhen-xing, ZHAO Bao-feng, XU Dong-hao, 2012. Sandbodies Frameworks of Subaqueous Distributary Channel in Shallow-Water Delta, Xinli Area of Songliao Basin. Earth Science, 37(3): 556-564. doi: 10.3799/dqkx.2012.062

Citation:

WANG Jia-hao, CHEN Hong-han, JIANG Tao, TANG Zhen-xing, ZHAO Bao-feng, XU Dong-hao, 2012. Sandbodies Frameworks of Subaqueous Distributary Channel in Shallow-Water Delta, Xinli Area of Songliao Basin. Earth Science, 37(3): 556-564. doi: 10.3799/dqkx.2012.062

Citation:

WANG Jia-hao, CHEN Hong-han, JIANG Tao, TANG Zhen-xing, ZHAO Bao-feng, XU Dong-hao, 2012. Sandbodies Frameworks of Subaqueous Distributary Channel in Shallow-Water Delta, Xinli Area of Songliao Basin. Earth Science, 37(3): 556-564. doi: 10.3799/dqkx.2012.062

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Sandbodies Frameworks of Subaqueous Distributary Channel in Shallow-Water Delta, Xinli Area of Songliao Basin

doi: 10.3799/dqkx.2012.062

1.
Key Laboratory of Tectonics and Petroleum Resources of Ministry of Education, China University of Geosciences, Wuhan 430074, China
2.
Petroleum Exploration and Production Research Institute of Jilin Oil Company Branch, CNPC, Songyuan 138000, China

Received Date: 2011-07-23
Available Online: 2021-11-09
Publish Date: 2012-05-01

Abstract

Abstract

The Songliao basin evolved into the late down-warping stage, and shallow-water deltas had extensively developed in the third Member of Nenjiang Formation, Upper Cretaceous. In the third member of the Xinli area, three depositional cycles were identified to be evolved from shallow-lake subfacies to delta front subfacies respectively, indicating gradually shallowing lake. Accordingly, three sand-units of Ⅲ, Ⅱ and Ⅰ were divided from the bottom to top. Based on abundant data of dense wells, sedimentary facies maps and sandbodies structures of subaqueous distributary channel in each sand-units were analyzed in detail, and a series of changes accompanied with basin flattening and shallowing gradually were summed up as follows: deltas farther extended; subaqueous distributary channels more stabilized; single channel farther elongated; channels less bifurcated and converged; crevasse splay occurred more frequently; subaqueous interdistributary bays distributed more extensively. Consequently subaqueous distributary channel sandbodies less connected with each other and can be described as moderately thick sheet-shaped, narrow-thin strap-shaped to speckle-shaped, and wide-thick strap-shaped respectively, which resulted in oil pools styles transforming from tectonic reservoirs to lithologic reservoirs. Finally, corresponding to the three sand-units respectively, three depositional models were summarized to be reticular, ramiform and meandering river-liking.
- Songliao basin,
- shallow-water delta,
- subaqueous distributary channel,
- lithologic reservoirs,
- petroleum geology

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References(34)

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Sandbodies Frameworks of Subaqueous Distributary Channel in Shallow-Water Delta, Xinli Area of Songliao Basin

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