钻孔岩心游离气对天然气水合物成因的指示意义

黄霞, 王平康, 肖睿, 庞守吉, 张帅, 祝有海. 钻孔岩心游离气对天然气水合物成因的指示意义[J]. 海洋地质与第四纪地质, 2017, 37(5): 82-89. doi: 10.16562/j.cnki.0256-1492.2017.05.008
引用本文: 黄霞, 王平康, 肖睿, 庞守吉, 张帅, 祝有海. 钻孔岩心游离气对天然气水合物成因的指示意义[J]. 海洋地质与第四纪地质, 2017, 37(5): 82-89. doi: 10.16562/j.cnki.0256-1492.2017.05.008
HUANG Xia, WANG Pingkang, XIAO Rui, PANG Shouji, ZHANG Shuai, ZHU Youhai. DETECTING GAS ORIGIN WITH FREE GAS FROM HYDRATE DRILLING CORE[J]. Marine Geology & Quaternary Geology, 2017, 37(5): 82-89. doi: 10.16562/j.cnki.0256-1492.2017.05.008
Citation: HUANG Xia, WANG Pingkang, XIAO Rui, PANG Shouji, ZHANG Shuai, ZHU Youhai. DETECTING GAS ORIGIN WITH FREE GAS FROM HYDRATE DRILLING CORE[J]. Marine Geology & Quaternary Geology, 2017, 37(5): 82-89. doi: 10.16562/j.cnki.0256-1492.2017.05.008

钻孔岩心游离气对天然气水合物成因的指示意义

  • 基金项目:
    国家自然科学基金项目(41202099)
详细信息
    作者简介: 黄霞(1982—),女,博士,副研究员,地质学专业,主要从事油气地质地球化学勘查研究,E-mail:huangxia@live.com
    通讯作者: 王平康(1982—),男,硕士,副研究员,沉积学专业,主要从事天然气水合物调查研究,E-mail:wangpk@cags.ac.cn
  • 中图分类号: P618.13

  • 周立君编辑

DETECTING GAS ORIGIN WITH FREE GAS FROM HYDRATE DRILLING CORE

More Information
  • 中国是世界上少数几个同时在海域和陆域冻土区取得天然气水合物找矿突破的国家,这为我国天然气水合物成矿气源研究提供了良好的研究条件。本文通过对南海神狐海域及祁连山冻土区不同层位、不同赋存状态的水合物气体数据进行分析,研究了各层位烃类气体的地球化学特征,并探讨其成因。研究结果表明,海域和陆域钻孔岩心游离气与水合物气具有基本一致的气体组分特征和同位素特征,表明气体成因类型相同。同一钻孔中,气体随埋深不同表现出不同的气体组分特征,甲烷碳同位素显示负偏,均表明气体存在垂向运移。岩心游离气对水合物成因类型判识具有指示意义,可作为判识水合物或潜在水合物成因类型的一种有效方法。

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  • 图 1  神狐海域水合物气和岩心游离气δ13C1与C1/(C2+C3)投点图

    Figure 1. 

    图 2  神狐海域水合物气和岩心游离气甲烷碳和氢同位素值投点图

    Figure 2. 

    图 3  祁连山冻土区不同层位水合物气和岩心游离气成因类型

    Figure 3. 

    图 4  陆域祁连山冻土区水合物钻孔R值随深度变化

    Figure 4. 

    表 1  南海神狐钻探区甲烷同位素及其烃类气体组分

    Table 1.  Methane isotope and C1/(C2+C3)value of samples from Shenhu area, South China Sea

    样品类型 样品编号 采样
    深度/m
    δ13C1
    /‰,PDB
    δD/‰,
    VSMOW
    C1/
    (C2+C3)
    水合物气 SH2B-12R 197~198 -56.7 -199 912
    SH3B-13P 190~191 -60.9 -191 1 094
    岩心游离气 SH3B-7P 123~124 -62.2 -225 1 374
    SH5C-11R 114~115 -54.1 -180 2 447
    下载: 导出CSV

    表 2  祁连山冻土区天然气水合物分布及样品采集信息

    Table 2.  Gas hydrate distribution in Qilian Mountain permafrost and samples information

    孔号 层位 深度/m 水合物层位 储集层主要岩性 水合物样品数 岩心游离气样品数
    DK-1 Ⅰ1 133.5~135.5 裂隙、孔隙型水合物层 细砂岩 1
    Ⅰ2 142.9~147.7 裂隙型水合物层 粉砂岩 1
    Ⅰ3 165.3~165.5 裂隙型水合物层 粉砂岩 1
    Ⅰ4 169.0~170.5 水合物异常层 粉砂岩
    DK-2 其他层 1 4
    Ⅱ1 144.4~152.0 裂隙、孔隙型水合物层 中砂岩,细砂岩 2 1
    Ⅱ2 152.3~156.6 裂隙型水合物层 油页岩
    Ⅱ3 235.0~291.3 裂隙型水合物层 油页岩,泥岩 8 1
    其他层 3 3
    Ⅱ4 377.3~387.5 水合物异常层 油页岩,中砂岩 1 1
    其他层 2
    DK-3 Ⅲ1 133.0~156.0 裂隙型水合物层 泥岩,油页岩 1
    Ⅲ2 225.1~240.0 裂隙型水合物层 泥岩,油页岩
    Ⅲ3 367.7~396.0 水合物异常层 细砂岩,粉砂岩 1
    DK-5 Ⅴ1 111.5~124.5 水合物异常层 泥岩,油页岩
    其他层 13
    Ⅴ2 231.56~234.46 水合物异常层 粉砂岩 1
    其他层 2
    Ⅴ3 274.0~310.0 水合物异常层 泥岩,粉砂岩,细砂岩 1
    其他层 10
    DK-6 其他层 4
    Ⅵ1 133.81~213.4 水合物异常层 泥岩,油页岩,粉砂岩 10
    Ⅵ2 245.8~280.0 水合物异常层 粉砂岩,油页岩 1
    DK-8 其他层 1
    Ⅷ1 147.8~155.93 水合物异常层 细砂岩 1
    其他层 1
    Ⅷ2 171.56~175.01 裂隙型水合物层 泥岩,油页岩
    其他层 1
    Ⅷ3 226.26~236.46 裂隙型水合物层 泥岩,油页岩
    Ⅷ4 265.94~291.24 裂隙、孔隙型水合物层 泥岩,油页岩,泥质粉砂岩 2
    Ⅷ5 301.84~304.28 水合物异常层 泥质粉砂岩
    下载: 导出CSV
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收稿日期:  2017-08-15
修回日期:  2017-08-30
刊出日期:  2017-05-28

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