Lithologic Reservoirs ›› 2022, Vol. 34 ›› Issue (6): 80-91.doi: 10.12108/yxyqc.20220607

• PETROLEUM EXPLORATION • Previous Articles     Next Articles

Sequence stratigraphic framework and platform margin belt distribution of Cambrian in northern Tarim Basin

LIU Yongli1, LI Guorong2, HE Zhao2, TIAN Jiaqi2, LI Xiaoxiao2   

  1. 1. Northwest Oilfield Company, Sinopec, Urumqi 830011, China;
    2. College of Energy, Chengdu University of Technology, Chengdu 610059, China
  • Received:2022-04-08 Revised:2022-06-11 Online:2022-11-01 Published:2022-11-09

Abstract: Based on the identification of key sequence boundaries,analysis of sequence duration,sedimentary facies division and analysis of stratigraphic superposition structure of Cambrian in northern Tarim Basin, the distribution of platform margin belt was sketched out with the third-order sequence as a unit, and its favorable exploration areas were defined. The results show that: (1)Ten third-order sequences were identified in the Cambrian strata in the northern Tarim Basin,and they were numbered from SQ1 to SQ10 from bottom to top. Gentle slope sediments are developed in the SQ1-SQ2 period of the Lower Cambrian, which are type Ⅰ sequences. In SQ3- SQ5 period,carbonate platforms of gentle slope are developed,which are type Ⅱ sequences. Carbonate platforms are developed in SQ6 period of Middle Cambrian,which are type Ⅱ sequences. Carbonate rimmed platforms are developed during SQ7- SQ10 period of Middle and Upper Cambrian. SQ 7 and SQ 9 are type Ⅰsequences,and SQ8 and SQ10 are type Ⅱ sequences.(2)The platform margin facies belt of SQ3 sequence in the study area shows wide spatial distribution. It is distributed along Keping uplift to Shaya uplift in near EW direction,and along Shaya uplift to Shuntuoguole uplift in near N-S direction. The platform margin facies belt of SQ4-SQ10 is distributed along N-S direction, showing good successive development characteristics, with the platform margin pushing towards the slope-basin area and displaying clear progradation pattern. High-energy reef shoal facies belt of SQ3-SQ10 is widely distributed, and the reef shoal facies reservoir area on the platform margin is large.(3)The platform margin facies belt in the study area extending in the N-S direction,located in the east of well TS2,is the most favorable zone for reservoir development. It is also the most favorable exploration area because of its good spatial relationship with Cambrian main source rocks.

Key words: third-order sequence, sequence stratigraphic framework, carbonate rock, tidal flat facies, reef shoal facies, lagoon facies, platform margin belt, Cambrian, northern Tarim Basin

CLC Number: 

  • TE122
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