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Geoscience ›› 2023, Vol. 37 ›› Issue (05): 1169-1181.DOI: 10.19657/j.geoscience.1000-8527.2022.093

• Sedimentology • Previous Articles     Next Articles

Development Model of Microbial Reef-shoal in the Lower Cambrian Xiaoerbulak Formation Under Transgression-Regression Transition in the Northern Tarim Basin

CHEN Gege1(), GAO Zhiqian1(), JIAO Cunli2, HU Zongquan2, YUAN Yuxuan1, WEI Duan1, ZHAI Xinqing1, CHANG Zhe1   

  1. 1. School of Energy, China University of Geosciences (Beijing), Beijing 100083, China
    2. Petroleum Exploration and Development Research Institute, SINOPEC, Beijing 100089, China
  • Received:2023-06-05 Revised:2023-06-29 Online:2023-10-10 Published:2023-11-14

Abstract:

Based on the outcrop observation in Aksu area in the northwestern Tarim Basin, and the analysis of logging data and thin section identification of key exploration wells there, the high-precision sequence stratigraphic framework at north Tarim Basin is established.We analyzed the development model of microbial reef-shoal and carbonate platform evolution in the Xiaoerbulak period, and suggested that the Xiaoerbulak Formation can be subdivided into two third-order sequences (SQ1 and SQ2) and five fourth-order sequences (sq1, sq2, sq3, sq4 and sq5): sq1 and sq2 developed layered microbial mats, which were middle-inner ramp deposition, corresponding to the ramp carbonate platform stage; sq3 is a transition period from ramp carbonate platform to slightly rimmed shelf carbonate platform, and the relative sea-level likely rose first and then fell, and microorganisms began to build reefs in the paleo-geomorphic highlands, and the microbiolites were basically undeveloped in the slope area of low paleo-geomorphic terrain; sq4 and sq5 represent the stage of slightly rimmed shelf carbonate platform with continuous sea-level decline; sq4 developed algal grain shoal and microbial reef deposits, whilst sq5 developed sand shoal, gravel shoal and microbial reef deposits.The high-precision sequence stratigraphic correlation shows that the sea-level change controlled the vertical development of microbial reef shoal, and the paleo-geomorphology controlled the planar microbial reef shoal distribution.

Key words: high-precision sequence division, stratigraphic framework, microbial reef-shoal, sedimentary facies, development model

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