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湖南弗拉阶地层的分布特征和页岩气有利区

王建坡, 王传尚, 吕嵘, 田巍. 2021. 湖南弗拉阶地层的分布特征和页岩气有利区[J]. 中国地质, 48(5): 1499-1509. doi: 10.12029/gc20210514
引用本文: 王建坡, 王传尚, 吕嵘, 田巍. 2021. 湖南弗拉阶地层的分布特征和页岩气有利区[J]. 中国地质, 48(5): 1499-1509. doi: 10.12029/gc20210514
WANG Jianpo, WANG Chuanshang, LÜ Rong, TIAN Wei. 2021. Distribution of the Frasnian strata in Hunan Province and shale gas prospects[J]. Geology in China, 48(5): 1499-1509. doi: 10.12029/gc20210514
Citation: WANG Jianpo, WANG Chuanshang, LÜ Rong, TIAN Wei. 2021. Distribution of the Frasnian strata in Hunan Province and shale gas prospects[J]. Geology in China, 48(5): 1499-1509. doi: 10.12029/gc20210514

湖南弗拉阶地层的分布特征和页岩气有利区

  • 基金项目:
    中国地质调查局项目(DD20160179,DD2019823)资助
详细信息
    作者简介: 王建坡, 男, 1981年生, 博士, 副研究员, 主要从事地层古生物及应用研究; E-mail: wangjianpo2001-1@163.com
  • 中图分类号: P541

Distribution of the Frasnian strata in Hunan Province and shale gas prospects

  • Fund Project: Supported by the project of China Geological Survey (No. DD20160179, No.DD2019823)
More Information
    Author Bio: WANG Jianpo, male, born in 1981, doctor, associate researcher, engaged in the study of stratigraphy, paleobiology and their applications; E-mail: wangjianpo2001-1@163.com .
  • 湖南上泥盆统弗拉阶佘田桥组泥页岩是重要的页岩气勘探目的层。由于区域上具有岩相分异显著、变化快的特征,佘田桥组存在多个同期地层,容易造成引用和野外识别困难,严重制约其页岩气调查工作进程。通过梳理佘田桥组及其同期地层的历史沿革,明确和圈定了它们的分布区域和使用范围。基于佘田桥组的岩石组合特征、有机碳含量的区域变化和已有调查成果,提出受陆缘碎屑输入影响较强的新化-涟源、邵东地区为页岩气有利勘探区的设想,同时认为找准台盆范围是页岩气调查发现的关键。

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  • 图 1  湖南弗拉阶佘田桥组沿革

    Figure 1. 

    图 2  湖南弗拉阶岩石地层组合及沉积相

    Figure 2. 

    图 3  湖南弗拉阶岩石地层柱状对比图

    Figure 3. 

    图 4  湖南弗拉期岩相古地理(古陆位置据Ma and Zong, 2010修改)

    Figure 4. 

    图 5  不同区域的佘田桥组岩石组合对比

    Figure 5. 

    图 6  二维地震反映的新化地区佘田桥组沉积期台盆范围

    Figure 6. 

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出版历程
收稿日期:  2019-07-11
修回日期:  2019-12-24
刊出日期:  2021-10-25

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