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2023 Vol. 50, No. 6
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Article navigation > Geology in China > 2023 > 50(6): 1848-1856
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JING Xigui, LI Fengjie, ZHANG Da, LI Ning, MIAO He, DING Rui. 2023. Nenjiang Formation 1 member Ichnocoenosis and its deposit environment of Upper Cretaceous from Yaonan 5 well, Songliao Basin[J]. Geology in China, 50(6): 1848-1856. doi: 10.12029/gc20200523001
Citation: JING Xigui, LI Fengjie, ZHANG Da, LI Ning, MIAO He, DING Rui. 2023. Nenjiang Formation 1 member Ichnocoenosis and its deposit environment of Upper Cretaceous from Yaonan 5 well, Songliao Basin[J]. Geology in China, 50(6): 1848-1856. doi: 10.12029/gc20200523001
shu

Nenjiang Formation 1 member Ichnocoenosis and its deposit environment of Upper Cretaceous from Yaonan 5 well, Songliao Basin

  • 1.

    Sinopec Northeast Oil and Gas Company, Changchun 130000, Jilin, China

  • 2.

    Institute of Sedimentary Geology, Chengdu University of Technology, Chengdu 610059, Sichuan, China

  • 3.

    Shandong Academy of Innovation Strategy, Jinan 250001, Shandong, China

    • Fund Project: Supported by Sinopec Science and Technology Department for the project "Study on the Evaluation of Oil and Gas Resource Potential and Areas Selection in Northeast China (No.P22062)"
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  • Author Bio: JING Xigui, male, born in 1992, master, assistant researcher, mainly engaged in the reservoir prediction; E-mail: 631407785@qq.com
  • Corresponding author: LI Fengjie, male, born in 1972, professor, doctoral supervisor, mainly engaged in the teaching and research of sedimentology and sequence stratigraphy; E-mail: lifengjie72@163.com 
Received Date:  23 May 2020
Revised Date:  11 July 2020
Publish Date:  25 December 2023
    Abstract

  • This paper is the result of oil and gas exploration engineering.

     Objective

    Abundant trace fossils were preserved in Upper Cretaceous strata in Songliao Basin, but related studies mainly focus on the northern part of the Songliao Basin. The sedimentary environment of section 1 of the Nenjiang Formation was restored by trace fossils identification in the southern part of the Songliao Basin, and this paper will provide evidence to support subsequent trace fossil studies in this area.

     Methods

    According toobserve wells of Yaonan 5 drill core of section 1 of the Nenjiang Formation, we identified 2 ichnogenus and 2 ichnospecies including Chondrites and Planolites, and established Chondrites-Planolites ichnocoenosis. Combining with ichnofossils surrounding rock, burrow scale, record of well logging curve to analyse trace maker habit; According well of Yaonan 5 sampling, measured sample contents of Uranium, Thorium, Vanadium, Nickel and Cobalt; Using U/Th, V/(V + Ni) and Ni/Co methods to restore trace fossil preservation strata paleo-oxygen facies of section 1 of the Nenjiang Formation.

     Results

    This study suggests that Chondrites-Planolites ichnocoenosis were formed in deep water environment with weak water energy; Paleo-oxigenation facies data analysis suggests that method of U/Th indicated oxic environment, methods ofV/(V + Ni) and Ni/Co indicated dysaerobic-anaerobic environment.

     Conclusions

    The trace fossils were preserved in mudstone in well Yaonan 5 with small burrow diameter scale and low abundance, indicating the water was anoxic. Combined with the paleooxygen facies data and logging curve analysis, considering that tracemaker were living in semi-deep lake which with low energy and poor oxygen content.
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