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滇东北DD1井五峰组—龙马溪组地层界线划分及沉积环境演变

冯伟明, 李嵘, 赵瞻, 余谦, 杨瀚, 谢渊, 叶定南. 2021. 滇东北DD1井五峰组—龙马溪组地层界线划分及沉积环境演变[J]. 中国地质, 48(1): 297-308. doi: 10.12029/gc20210120
引用本文: 冯伟明, 李嵘, 赵瞻, 余谦, 杨瀚, 谢渊, 叶定南. 2021. 滇东北DD1井五峰组—龙马溪组地层界线划分及沉积环境演变[J]. 中国地质, 48(1): 297-308. doi: 10.12029/gc20210120
FENG Weiming, LI Rong, ZHAO Zhan, YU Qian, YANG Han, XIE Yuan, YE Dingnan. 2021. Boundary definition of Wufeng Formation and Longmaxi Formation in well DD1 and sedimentary environment evolution of Northeastern Yunnan[J]. Geology in China, 48(1): 297-308. doi: 10.12029/gc20210120
Citation: FENG Weiming, LI Rong, ZHAO Zhan, YU Qian, YANG Han, XIE Yuan, YE Dingnan. 2021. Boundary definition of Wufeng Formation and Longmaxi Formation in well DD1 and sedimentary environment evolution of Northeastern Yunnan[J]. Geology in China, 48(1): 297-308. doi: 10.12029/gc20210120

滇东北DD1井五峰组—龙马溪组地层界线划分及沉积环境演变

  • 基金项目:
    国家科技重大专项“页岩气勘查评价技术试验与应用推广”(2016ZX05034-004)、中国地质调查局地质调查二级项目“四川盆地下古生界海相页岩气基础地质调查”(DD20160176)、“滇东北地区页岩气地质调查”(DD20190080)联合资助
详细信息
    作者简介: 冯伟明, 男, 1986年生, 硕士, 高级工程师, 主要从事沉积学与石油天然气地质学方面研究; E-mail:fengweiming009@163.com
    通讯作者: 李嵘, 男, 1967年生, 教授级高级工程师, 主要从事石油天然气地质学方面研究; E-mail:545210420@qq.com
  • 中图分类号: P534.42-43;P512.2

Boundary definition of Wufeng Formation and Longmaxi Formation in well DD1 and sedimentary environment evolution of Northeastern Yunnan

  • Fund Project: Supported by National Science and Technology Major Project (No.2016ZX05034-004) and the project of China Geology Survey(No.DD20160176, No.DD20190080)
More Information
    Author Bio: FENG Weiming, male, born in 1986, master, senior engineer, engaged in sedimentology and oil & gas geological survey and research; E-mail:fengweiming009@163.com .
    Corresponding author: LI Rong, male, born in 1967, bachelor, senior engineer, engaged in oil and gas geological research; E-mail:545210420@qq.com
  • DD1井上奥陶统临湘组泥灰岩之上发育大套粉砂质泥岩,笔石化石缺乏,也未发现观音桥段含赫南特贝灰岩标志层,O-S界线通过生物地层和岩石地层方法难以确定。微量、稀土元素分析表明,粉砂质泥岩中部(1288.3 m)的Th、Sr、Y、Th/U以及Cen、EunδCe、δEu曲线均呈现尖锐的异常峰,该处∑REE含量显著高于上下地层,REE分布曲线右倾斜率更大。将DD1井与扬子地区其他O-S界线剖面的元素地球化学特征进行对比分析,可判断DD1井存在五峰组观音桥段,该标志层的厚度也小于1 m。微量元素地球化学氧化-还原判别图还表明,五峰期-龙马溪期早期沉积水介质主要处于弱氧化环境,观音桥期氧化性达到最强;根据沉积学标志分析,O-S之交沉积相演变过程为:潮下→潮间→潮上→潮间,在观音桥期水体最浅,为潮上带沉积。

  • 加载中
  • 图 1  DD1井地质背景图

    Figure 1. 

    图 2  奥陶系—志留系界线附近敏感微量元素地球化学异常分布曲线对比图

    Figure 2. 

    图 3  DD1井奥陶系—志留系界线附近Cen, EunδCe, δEu曲线对比

    Figure 3. 

    图 4  DD1井奥陶系-志留系界线附近稀土元素分配模式图

    Figure 4. 

    图 5  DD1井上奥陶统五峰组-下志留统龙马溪组下段氧化还原环境的微量元素判别指标(①~⑤分别代表①小段~⑤小段)

    Figure 5. 

    图 6  DD1井奥陶统五峰组—下志留统龙马溪组下段发育的沉积标志

    Figure 6. 

    表 1  DD1井部分代表性样品主量、微量和稀土元素含量及比值(主量元素单位为%;其他元素为μg/g)

    Table 1.  Contents and ratios of trace elements, REE(μg/g) and major elements(%)in some samples of well DD1

    下载: 导出CSV
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出版历程
收稿日期:  2018-08-06
修回日期:  2018-09-30
刊出日期:  2021-02-25

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