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    济阳坳陷细粒混积岩类型与湖盆演化的耦合关系

    马义权 刘惠民 张守鹏 陆永潮 刘晓峰

    马义权, 刘惠民, 张守鹏, 陆永潮, 刘晓峰, 2020. 济阳坳陷细粒混积岩类型与湖盆演化的耦合关系. 地球科学, 45(10): 3633-3644. doi: 10.3799/dqkx.2020.192
    引用本文: 马义权, 刘惠民, 张守鹏, 陆永潮, 刘晓峰, 2020. 济阳坳陷细粒混积岩类型与湖盆演化的耦合关系. 地球科学, 45(10): 3633-3644. doi: 10.3799/dqkx.2020.192
    Ma Yiquan, Liu Huimin, Zhang Shoupeng, Lu Yongchao, Liu Xiaofeng, 2020. Types of Fine-Grained Mixed Sedimentary Rocks of Shahejie Formation and Evolution of Lake Basin in Jiyang Depression, Eastern China. Earth Science, 45(10): 3633-3644. doi: 10.3799/dqkx.2020.192
    Citation: Ma Yiquan, Liu Huimin, Zhang Shoupeng, Lu Yongchao, Liu Xiaofeng, 2020. Types of Fine-Grained Mixed Sedimentary Rocks of Shahejie Formation and Evolution of Lake Basin in Jiyang Depression, Eastern China. Earth Science, 45(10): 3633-3644. doi: 10.3799/dqkx.2020.192

    济阳坳陷细粒混积岩类型与湖盆演化的耦合关系

    doi: 10.3799/dqkx.2020.192
    基金项目: 

    国家自然科学基金青年科学基金项目 41802175

    中国博士后科学基金 2019M650184

    国家科技重大专项 2017ZX05049-004

    详细信息
      作者简介:

      马义权(1988-), 男, 讲师, 博士后, 主要从事非常规油气储层非均质性研究.ORCID:0000-0002-0937-9366.E-mail:yqma88@163.com

    • 中图分类号: P624

    Types of Fine-Grained Mixed Sedimentary Rocks of Shahejie Formation and Evolution of Lake Basin in Jiyang Depression, Eastern China

    • 摘要: 综合钻井、岩心、薄片和地球化学等资料,详细研究了济阳坳陷沾化凹陷沙三段下亚段细粒混积岩的混积类型、不同类型细粒混积岩的成因、垂向分布以及古湖泊水文演化规律.结果表明,沾化凹陷沙三段下亚段细粒混积岩包括层状-纹层状组构混积型和块状矿物组分混积型等2种混积类型;自下而上主要由层状-纹层状组构混积型夹块状矿物组分混积型发育段,过渡为块状矿物组分混积型夹层状-纹层状组构混积型发育段;表明了由潮湿且受季节性气候影响明显的深水湖泊,演化为水体较浅、盐度均一且受季节性气候影响不明显的湖泊环境,并建立了高水位早期-高水位中-晚期-低水位期的湖泊演化模式.在湖泊高水位早期阶段的早-中期和高水位中-晚期,有机质富集的主控因素主要是氧化还原条件和古生产力;在湖泊高水位早期阶段的晚期,古生产力是有机质富集的主控因素;在湖泊低水位时期,有机质富集的主控因素是氧化还原条件.总体上,适量的陆源供给(粘土矿物和石英含量均小于22%)会促进有机质富集,而过量的陆源碎屑输入以及碳酸盐的快速沉淀都会导致有机质被稀释.

       

    • 图  1  济阳坳陷构造地质简图(a);沾化凹陷南北向构造单元组成及主要沉积地层分布(b);沾化凹陷古近系-新近系地层分布简图(c)

      图a据Jiu et al. (2013)Wang et al. (2015)修改;图b据Jiu et al. (2013)Wang et al. (2015)修改;图c据Feng et al. (2016)修改

      Fig.  1.  Distribution of geological tectonic units in the Jiyang Depression with the locations of L69 well and the location of cross-section SN (a); N-S cross-section of the Zhanhua Depression showing tectonic-structural zones and stratigraphic intervals (b); General Paleogene-Neogen stratigraphy of the Zhanhua Depression (c)

      图  2  L69井沙三段下亚段细粒混积岩类型、TOC含量、主要矿物含量和地球化学参数垂向序列

      Fig.  2.  Types of fine-grained mixed sedimentary rocks, TOC, mineral composition and geological index variation of the lower submember of Es3 in the L69 well

      图  3  沾化凹陷沙三下亚段细粒混积岩沉积特征

      a~e.层状-纹层状组构混积型;a.纹层结构;b.植物叶片化石(箭头);c.平行且连续的纹层;d.韵律变化的隐晶方解石透镜体(白色箭头)和富粘土质纹层(黄色箭头);e.鱼骨化石的横截面;f~j.块状组分混积型;f~g.块状组分混积型与层状-纹层状组构混积型明显分界;h.介形虫化石略具定向性,可见次棱角-次圆状石英粉砂;i.介形虫碎片无序分布,石英粉砂主要呈次棱角状;j.隐晶质方解石与粘土矿物较均匀混合

      Fig.  3.  Characteristic of sedimentary observations of the fine-grained mixed sedimentary rocks of the lower submember of Es3 in Zhanhua Depression

      图  4  沾化凹陷沙三段下亚段湖泊演化模式

      Fig.  4.  Lake evolution model for the lower submember of Es3 in Zhanhua Depression

      图  5  石英和粘土矿物含量分别与TOC含量的相关性

      Fig.  5.  Correlations quartz and clay contents vs. TOC content of the lower submember of Es3 in the L69 well

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