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松辽盆地腰南5井上白垩统嫩江组一段遗迹化石组合及其沉积环境

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荆锡贵, 李凤杰, 张达, 李宁, 苗贺, 丁锐. 2023. 松辽盆地腰南5井上白垩统嫩江组一段遗迹化石组合及其沉积环境[J]. 中国地质, 50(6): 1848-1856. doi: 10.12029/gc20200523001
引用本文: 荆锡贵, 李凤杰, 张达, 李宁, 苗贺, 丁锐. 2023. 松辽盆地腰南5井上白垩统嫩江组一段遗迹化石组合及其沉积环境[J]. 中国地质, 50(6): 1848-1856. doi: 10.12029/gc20200523001
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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
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松辽盆地腰南5井上白垩统嫩江组一段遗迹化石组合及其沉积环境

  • 1.

    中国石油化工股份有限公司东北油气分公司, 吉林 长春 130000

  • 2.

    成都理工大学沉积地质研究院, 四川 成都 610059

  • 3.

    山东省创新战略研究院, 山东 济南 250001

  • 基金项目:
    中国石油化工股份有限公司科技部项目“东北地区油气资源潜力与选区评价研究（P22062）”资助
详细信息
    作者简介: 荆锡贵, 男, 1992年生, 硕士, 助理研究员, 从事储层预测工作; E-mail: 631407785@qq.com
    通讯作者: 李凤杰, 男, 1972年生, 教授, 博士生导师, 沉积学专业, 从事沉积学与层序地层学方面的教学与研究工作; E-mail: lifengjie72@163.com

  • 中图分类号: P618.13

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)"
More Information
    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

    摘要
  • 研究目的

    松辽盆地上白垩统嫩江组中含有丰富的遗迹化石，但相关研究主要集中于松辽盆地北部。通过鉴定遗迹化石还原松辽盆地南部嫩江组一段沉积环境，为该地区后续遗迹化石研究提供证据支持。

     研究方法

    通过观察腰南5井嫩江组一段岩心，发现了Chondrites及Planolites等共计2属，2种遗迹化石，建立了Chondrites-Planolites遗迹化石组合；结合遗迹化石围岩岩性、潜穴规模、测井曲线记录对造迹生物生存习性进行分析；通过腰南5井采样，分析样品中铀、钍、钒、镍与钴含量，使用铀/钍、钒（/钒+镍）与镍/钴等手段对嫩一段遗迹化石保存层位的古氧相进行还原。

     研究结果

    研究认为Chondrites-Planolites遗迹化石组合形成于水动力较小的深水环境；古氧相数据分析表明，腰南5井嫩一段泥岩样品铀/钍指示常氧环境，钒（/钒+镍）与镍/钴指示贫氧-缺氧环境。

     结论

    腰南5井嫩一段遗迹化石组合保存于泥岩且潜穴直径小，遗迹化石丰度低，表明水体含氧量低。结合古氧相数据和测井曲线分析，认为造迹生物的生活环境为水动力较弱且水体氧含量低的半深湖相环境。

    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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  • 图 1  研究区域示意图（据郑玉龙等，2005修改）

    Figure 1. 

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    图 2  松辽盆地嫩一段沉积相分布示意图（据冯志强等，2012修改）

    Figure 2. 

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    图 3  腰南5井嫩江组一段沉积柱状图及遗迹化石分布

    Figure 3. 

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    图 4  腰南5井嫩江组一段化石、遗迹化石及岩心照片

    Figure 4. 

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    图 5  遗迹相及其环境分布模式图（据Seilacher，1967修改）

    Figure 5. 

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    表 1  嫩江组一段古氧相地球化学指标对比（据施春华等，2004）

    Table 1.  Geochemical indexes of paleo-oxygenation facies of K2n1(modified from Shi Chunhua et al., 2004)

    下载: 导出CSV

    表 2  腰南5井嫩一段泥岩地球化学数据分析

    Table 2.  Shale paleo-oxygenation facies geochemical data analysis of K2n1 from well Yaonan 5

    下载: 导出CSV
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收稿日期:  2020-05-23
修回日期:  2020-07-11
刊出日期:  2023-12-25

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