留言板

尊敬的读者、作者、审稿人, 关于本刊的投稿、审稿、编辑和出版的任何问题, 您可以本页添加留言。我们将尽快给您答复。谢谢您的支持!

姓名
邮箱
手机号码
标题
留言内容
验证码

珠江口盆地白云-荔湾深水区幔源CO2充注的黏土矿物成岩响应

刘妍鷨 陈红汉 王艳飞 韩晋阳 李倩

刘妍鷨, 陈红汉, 王艳飞, 韩晋阳, 李倩. 珠江口盆地白云-荔湾深水区幔源CO2充注的黏土矿物成岩响应[J]. 地质科技通报, 2021, 40(3): 85-95. doi: 10.19509/j.cnki.dzkq.2021.0020
引用本文: 刘妍鷨, 陈红汉, 王艳飞, 韩晋阳, 李倩. 珠江口盆地白云-荔湾深水区幔源CO2充注的黏土矿物成岩响应[J]. 地质科技通报, 2021, 40(3): 85-95. doi: 10.19509/j.cnki.dzkq.2021.0020
Liu Yanhua, Chen Honghan, Wang Yanfei, Han Jinyang, Li Qian. Diagenetic effect of mantle-derived CO2 charge to clay minerals in the Baiyun-Liwan deepwater area of the Pearl River Mouth Basin in South China Sea[J]. Bulletin of Geological Science and Technology, 2021, 40(3): 85-95. doi: 10.19509/j.cnki.dzkq.2021.0020
Citation: Liu Yanhua, Chen Honghan, Wang Yanfei, Han Jinyang, Li Qian. Diagenetic effect of mantle-derived CO2 charge to clay minerals in the Baiyun-Liwan deepwater area of the Pearl River Mouth Basin in South China Sea[J]. Bulletin of Geological Science and Technology, 2021, 40(3): 85-95. doi: 10.19509/j.cnki.dzkq.2021.0020

珠江口盆地白云-荔湾深水区幔源CO2充注的黏土矿物成岩响应

doi: 10.19509/j.cnki.dzkq.2021.0020
详细信息
    作者简介:

    刘妍鷨(1989-), 女, 现正攻读矿产普查与勘探专业博士学位, 主要从事含烃流体地质方面的研究工作。E-mail: liuyanhua@cug.edu.cn

    通讯作者:

    陈红汉(1962-), 男, 教授, 博士生导师, 主要从事油气成藏过程和流体包裹体系统分析方面的研究工作。E-mail: hhchen@cug.edu.cn

  • 中图分类号: P588.22

Diagenetic effect of mantle-derived CO2 charge to clay minerals in the Baiyun-Liwan deepwater area of the Pearl River Mouth Basin in South China Sea

  • 摘要: 珠江口盆地白云-荔湾深水区油气勘探中钻遇大量高含量CO2气层,使得如何规避高CO2风险成为当前面临的挑战。通过工区充注CO2的储层砂岩黏土矿物X射线衍射(XRD)、流体包裹体显微测温和稀有气体同位素组成等分析,明确了幔源无机CO2的成因,并运用黏土矿物特征讨论高温幔源无机CO2充注的黏土矿物成岩响应:有序带倒转和大量自生高岭石的生成。依据CO2气井的XRD全定量分析数据剖面图将幔源无机CO2气层段的黏土矿物组合分为3类:Ⅰ类为I/S混层黏土矿物中S体积分数介于10%~25%之间,有序度处于R2~R3带,高岭石体积分数高;Ⅱ类为I/S混层黏土矿物中S体积分数介于10%~15%,有序度为R2~R3带,自生高岭石体积分数低;Ⅲ类为I/S混层黏土矿物中S体积分数介于50%~60%,有序度为R0带,高岭石体积分数低。总结出幔源CO2在珠江组和珠海组中存在2种运聚模式:一是幔源CO2通过与基性岩浆连通的深大断裂垂直向上运聚;二是垂直向上运移后通过连通砂体侧向长距离运聚。研究结果对珠江口盆地白云-荔湾深水区下一步油气勘探规避高含量CO2风险具有指导作用。

     

  • 图 1  珠江口盆地白云-荔湾深水区构造区划图及采样井分布

    Figure 1.  Map of structural units division and distribution of samples in Baiyun-Liwan deepwater area, PRMB

    图 2  珠江口盆地白云-荔湾深水区天然气中3He/4He-δ13CCO2-PDB关系图(底图据文献[25])

    Figure 2.  Plot of 3He/4He-δ13CCO2-PDB of the natural gas samples in Baiyun-Liwan deepwater area, PRMB

    图 3  珠江口盆地白云-荔湾深水区天然气CO2/3He-δ13CCO2-PDB关系图(底图据文献[25])

    Figure 3.  Plot of CO2/3He-δ13CCO2-PDB of the natural gas samples in Baiyun-Liwan deepwater area, PRMB

    图 4  珠江口盆地深水区P5井砂岩岩屑样品(穿石英颗粒裂纹中)检测到含CO2盐水包裹体及其伴生的气液两相盐水包裹体

    Figure 4.  Roman spectrogram of CO2 inclusions and photomicrographs of CO2 inclusions and their coeval aqueous inclusions, plane polarized light in the PRMB

    图 5  珠江口盆地深水区流体包裹体均一温度频率直方图

    Figure 5.  Histogram of homogenization temperatures of fluid inclusions in deepwater area of the PRMB

    图 6  高含CO2井区单井XRD分析黏土矿物质量分数-深度剖面图

    a.P5井,2 836.2~2 912 m为含CO2层段,φ(CO2)为14.00%~16.10%;b.P6、P7、P8井,2 733~2 903.5 m为含CO2层段,φ(CO2)为8.47%~9.00%;c.P11井,3 612~3 820 m为含CO2层段,φ(CO2)为7.67%~58.50%;d.W14井,3 184.9~3 189 m、3 321.2~3 370.1 m为含CO2层段,φ(CO2)分别为59.36%~62.16%、85.75%~92.41%

    Figure 6.  Cross plots of clay mineral contents-depth for the single well XRD in deepwater area

    图 7  白云-荔湾深水区CO2气层砂岩样品SEM照片

    a.长石发生溶蚀作用;b.孔隙间充填假六方板状自生高岭石;c.孔隙间生成自生石英

    Figure 7.  SEM photograph of sandstone samples of CO2 gas reservoir in Baiyun-Liwan deepwater area

    图 8  含CO2的岩屑长石砂岩中自生碳钠铝石矿物岩石学照片

    a.W14井,3 156.4 m,正交偏光,碳钠铝石交代有孔虫体腔壁;b.W14井,3 156.4 m,正交偏光,碳钠铝石沿有孔虫体腔壁向体腔中心发育;c.W14井,3 239.1 m,扫描电镜(SEM),粒间孔隙生长的纤维状碳钠铝石;d.P9井,2 516.72 m,正交偏光,粒间孔隙中的碳钠铝石

    Figure 8.  Petrological photographs of dawsonites developed in the bearing CO2 debris-arkosic sandstones

    图 9  深水区砂岩粒间孔隙充填方解石、白云石和Fe-白云石胶结物的透射光、阴极光照片

    a, b.P13井,3 372.6~3 372.75 m,粗砂岩,粒间孔隙充填大量发桔红色阴极光的含铁方解石胶结物;c, d.L2井,2 196.0~2 196.15 m,极细粉砂岩,充填暗棕色阴极光的铁方解石脉;e, f.L18井,3 440.59 m,细砂岩,粒间孔隙充填发桔黄色阴极光的含铁方解石胶结物和发桔黄色阴极光的粒状白云石,白云石多为菱形自形,可见环带结构;g, h.L11井,2 878 m,砂岩,粒间孔隙充填发暗棕色阴极光的粒状白云石,白云石多为菱形自形,可见环带结构

    Figure 9.  Transmission and cathodic photographs of intergranular pores of sandstone filled with calcite, dolomite and Fe-dolomite cement in deepwater area

    图 10  白云-荔湾深水区温度-方解石胶结物δ18O关系图(底图据文献[7])

    Figure 10.  Scatter diagram between homogenization temperature and δ18O of aqueous inclusion in in the carbonte cements of Zhuhai and Zhujiang Formations in deepwater area

    图 11  珠江口盆地白云-荔湾深水区幔源CO2运移聚集模式图

    Figure 11.  Geological cross sections of the deepwater area of PRMB illustrating the migration and accumulation of mantle-derived CO2 gas

    表  1  珠江口盆地白云-荔湾深水区CO2及稀有气体同位素和体积分数分析结果

    Table  1.   Concentrations and isotopic of CO2 and rare gases in Baiyun-Liwan deepwater area, PRMB

    井号 深度/m φ(CO2)/% δ13CCO2-PDB/‰ 3He/4He CO2/3He 幔源He贡献率/%
    L11 1 502.0 0.56 -2.4 2.17 3.36×107 26.94
    L13 1 763.6 0.96 -5.7 2.22 5.41×107 27.57
    L18 2 511.5 4.46 -3.2 1.14 6.48×108 14.04
    W14 1 907.3 3.98 -4.1 2.18 3.72×108 27.07
    W14 2 249.0 9.00 -4.2 2.18 1.18×109 27.07
    W11 3 192.0 3.89 -4.6 1.21 7.42×108 14.91
    P4 2 711~2 766 3.81 -3.3 1.70 3.27×108 21.05
    P5 2 743~2 758 3.38 -3.2 1.76 2.45×108 21.80
    P5 3 249.0 11.84 -3.8 1.30 3.08×109 16.04
    P11 2 111.0 97.92 -4.8 5.90 1.88×109 73.65
    P11 2 111.0 98.27 -6.5 6.59 7.10×109 82.31
    P14 3 189.4 60.11 -5.0 6.92 3.57×108 86.42
    P14 3 321.2 85.75 -3.9 6.51 2.46×108 81.30
    L11 3 370.1 90.09 -1.2 6.86 6.70×108 85.76
    注:取国际公认值空气标准:Ra=(1.40±0.03)×10-6w(4He)=5.24×10-6;幔源He贡献率(%)=(R-R)/(R-R),式中,R为壳源中3He/4He(R=0.02Ra);R为测试样品中3He/4He值(R=(8±1)Ra),Ra为大气中3He/4He值
    下载: 导出CSV

    表  2  白云-荔湾深水区流体包裹体均一温度及现今地层温度

    Table  2.   Homogenization temperature of fluid inclusions and current formation temperature in Baiyun-Liwan deepwater area

    井号 深度/m 层位 CO2包裹体
    均一温度
    ThCO2/℃
    伴生盐水
    包裹体均一
    温度Th/℃
    现今地
    层温度
    T/℃
    L1 2 169~2 172 N1z 29.3 136.1 100.0
    L11 2 883 N1z 27.7 112.9 103.6
    L13 2 722 N1z 33.8 140.4 107.4
    L18 3 791 E3z 32.5 170.3 162.4
    L18 3 804.98 E3z 27.9 189.9 163.1
    W14 3 385 E3z 31.4 194.7 165.8
    W14 3 397 E3z 29.7 197.8 166.4
    W11 3 270 E3z 29.3 210.4 192.3
    P4 3 005 N1z 29.3 160.8 121.1
    P5 2 838 N1z 30.7 130.3 104.9
    P5 2 859 N1z 29.4 130.5 105.7
    P11 3 367 N1z 29.5 167.2 134.4
    P14 3 776.5 N1z 32.5 174.2 149.5
    P14 3 765 N1z 29.8 187.0 149.1
    P14 3 765 N1z 28.8 176.7 149.1
    注:N1z.珠海组;E3z.珠江组
    下载: 导出CSV

    表  3  珠江口盆地白云-荔湾深水区自生高岭石含量、黏土矿物有序带及CO2稳定同位素统计表

    Table  3.   Data of authigenic kaolinite contents, S% and the orders in I/S mixed clay minerals, and natural gas components contents and stable carbon isotopic ratios of CO2

    井号 深度/m 层位 岩性 高岭石
    wB/%
    I/S中S
    wB/%
    有序带 黏土矿物
    组合类型
    CH4 CO2 N2 δ13C1-PDB/
    δ13C2-PDB/
    δ13C3-PDB/
    δ13CnC4-PDB/
    δ13CnC5-PDB/
    δ13CCO2-PDB/
    φB/%
    L4 2 725~2 748 N1z2 砂岩 76.80 10 R3 88.660 3.570 0.33 -36.70 -26.85 -25.61 -25.01 -7.89
    L16 2 372~2 374.5 N1z2 砂岩 23.70 25 R2 89.44 2.52 0.98 -38.20 -28.40 -27.30 -27.00 -25.40 -8.40
    L16 2 471~2 513.5 N1z2 砂岩 42.40 25 R2 90.33 3.29 0.84 -37.10 -29.20 -26.40 -26.00 -24.90 -9.50
    L20 2 976.5~2 990.28 N1z2 砂岩 43.30 25 R2 87.50 3.98 0.48 -39.10 -29.10 -28.30 -27.60 -25.90 -9.10
    L20 3 006.8~3 008.2 N1z2 砂岩 53.70 25 R2 88.48 3.42 0.16 -39.00 -28.40 -27.70 -27.20 -26.00 -8.20
    W14 3 184.9~3 189.4 N1z 砂岩 37.00 10 R3 35.04 62.16 1.73 -51.10 -34.00 -30.10 -28.40 -4.80
    W14 3 321.0~3 321.2 N1z 砂岩 34.00 10 R3 12.29 87.61 0.00 -53.20 -34.90 -30.20 -27.70 -2.90
    W14 3 354.3~3 370.1 E3z 砂岩 64.00 10 R3 5.74 91.77 2.27 -52.90 -35.10 -30.40 -28.60 -3.20
    P5 2 904~2 912 泥质细砂岩 77.00 10 R3 5.29 2.69 91.70 -34.40 -28.50 -29.90 -7.20
    P7 1 727~1 728.7 N1z1 中粗砂岩 67.50 25 R2 87.70 1.57 4.33 -35.80 -25.40 -26.40 -8.40
    P7 2 903~2 903.5 细砂岩 78.50 15 R2 85.20 3.79 3.44 -36.70 -29.70 -28.90 -5.10
    P6 1 907.3~1 917.0 粉-细砂岩 48.00 20 R2 89.91 4.41 0 -38.10 -29.20 -27.90 -27.60 -27.40 -6.30
    P6 2 249 N1h 粉-细砂岩 53.00 25 R2 85.60 8.47 0 -36.80 -29.30 -28.20 -27.50 -27.60 -6.20
    P9 2 711~2 726 N1z2 砂岩 52.70 15 R2 88.58 4.10 0.57 -35.50 -28.80 -27.20 -26.70 -26.50 -4.50
    P9 2 743~2 758 N1z2 砂岩 76.88 15 R2 89.13 3.94 0.46 -36.90 -28.80 -27.70 -27.50 -27.30 -5.40
    P13 3 281 N1z2 灰质细砂岩 24.00 20 R2 84.37 7.41 0.50 -37.66 -28.96 -26.85 -26.16 0 -3.25
    P13 3 313.5 N1z2 粉砂岩 38.00 20 R2 88.03 4.63 0.07 -37.61 -29.10 -27.44 -26.64 0 -5.12
    P13 3 329 N1z2 细砂岩 30.00 20 R2 90.28 3.45 4.24 -37.24 -29.15 -27.09 -26.33 0 -4.82
    P16 3 230~3 238.5 N1z2 细砂岩 73.75 15 R2 78.09 14.56 0.11 -36.38 -28.07 -26.26 -26.65 -25.59 -4.22
    P20 4 055.6~4 056.3 N1z2 粉砂岩 10.00 15 R2 75.78 18.50 0.09 -35.60 -28.50 -26.90 -25.80 0 -2.50
    P11 3 612~3 632.8 N1z2 细砂岩 0.00 15 R2 80.00 13.80 0.43 -34.60 -27.70 -27.00 0 0 -2.50
    P11 3 650~3 660 N1z2 细砂岩 1.00 15 R2 78.80 13.80 0.61 -36.80 -28.60 -27.40 0 0 -4.70
    P15 3 242~3 249 N1z 细砂岩 3.00 15 R2 82.19 11.91 0.03 -35.90 -29.10 -27.80 -27.10 -26.60 -5.00
    W10 2 111.5~2 116.5 E3z 砂岩 3.00 50~60 R0 2.16 93.95 3.89 -35.71 -26.87 -23.77 0 0 -6.47
    注:N1h为韩江组
    下载: 导出CSV

    表  4  W14井岩屑长石砂岩XRD分析结果[26]

    Table  4.   XRD measurement of debris-arkosic sandstones in Well W14

    深度/m 层位 矿物wB/%
    石英 钾长石 方解石 白云石 菱铁矿 黄铁矿 碳钠铝石
    3 109~3 112 珠江组 29.0 1.4 1.4 27.8 5.7 - -
    3 277~3 280 珠江组 41.2 1.9 - 5.3 0.9 3.0 0.3
    3 331~3 334 珠江组 63.7 4.2 - 3.1 3.3 1.0 -
    3 379~3 382 珠海组 73.9 1.9 - 1.2 3.7 1.5 -
    3 475~3 478 珠海组 67.4 - - 0.8 3.1 0.9 0.8
    3 646~3 649 恩平组 41.5 - 1.0 3.3 3.2 2.9 -
    3 916~3 919 文昌组 44.6 2.7 13.9 3.8 - 0.4 -
    注:“-”代表含量微少;样品测试在吉林大学测试科学实验中心完成
    下载: 导出CSV
  • [1] Eberl D, Hower J. Kinetics of illite formation[J]. Geological Society of America Bulletin, 1976, 87(2): 1326-1330. http://bulletin.geoscienceworld.org/content/87/9/1326
    [2] Yun J, Wu H, Feng Z, et al. CO2 gas emplacement age in the Songliao Basin: Insight from volcanic quartz 40Ar-39Ar stepwise crushing[J]. Science Bulletin, 2010, 55(17): 1795-1799. doi: 10.1007/s11434-010-3082-y
    [3] Bethke C M, Vergo N, Altaner S P. Pathways of smectite illitization[J]. Clays and Clay Minerals, 1986, 34(2): 125-135. doi: 10.1346/CCMN.1986.0340203
    [4] Hoffman J, Hower J. Clay mineral assemblages as low grade metamorphic geothermometers: Application to the thrust faulted disturbed belt of Montana, U.S. A[M]. Oklahoma: SEPM Special Publications, 1979.
    [5] Hower J, Eslinger E V, Hower M E, et al. Mechanism of burial metamorphism of argillaceous sediment: 1. Mineralogical and chemical evidence[J]. Geological Society of America Bulletin, 1976, 87(5): 725-737. doi: 10.1130/0016-7606(1976)87<725:MOBMOA>2.0.CO;2
    [6] Moore D M, Reynolds R C. X-ray diffraction and the identification and analysis of clay minerals[M]. New York: Oxford University Press, 1989.
    [7] Davies G R, Smith L B. Structurally controlled hydrothermal dolomite reservoir facies: An overview[J]. AAPG Bulletin, 2011, 90(11): 1641-1690. http://www.nrcresearchpress.com/servlet/linkout?suffix=rg11/ref11&dbid=16&doi=10.1139%2FE09-019&key=10.1306%2F05220605164
    [8] 陈红汉, 米立军, 刘妍鷨, 等. 珠江口盆地深水区CO2成因、分布规律与风险带预测[J]. 石油学报, 2017, 38(2): 119-134. https://www.cnki.com.cn/Article/CJFDTOTAL-SYXB201702001.htm

    Chen H H, Mi L J, Liu Y H, et al. Genesis, distribution and risk belt prediction of CO2 in deep-water area in the Pearl River Mouth Basin[J]. Acta Petrolei Sinica, 2017, 38(2): 119-134(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-SYXB201702001.htm
    [9] 张鑫, 陈红汉, 龙昭, 等. 泌阳凹陷北部缓坡带核桃园组油气运聚成藏过程[J]. 地质科技通报, 2020, 39(3): 140-149. https://www.cnki.com.cn/Article/CJFDTOTAL-DZKQ202003018.htm

    Zhang X, Chen H H, Long Z, et al. Hydrocarbon migration and accumulation of Hetaoyuan Formation in the northern gentle slope of Biyang Depression[J]. Bulletin of Geological Science and Technology, 2020, 39(3): 140-149(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-DZKQ202003018.htm
    [10] 李智, 张志业, 何登发, 等. 南襄盆地泌阳凹陷与南阳凹陷油气地质特征类比及勘探启示[J]. 地质科技通报, 2020, 39(2): 79-89. https://www.cnki.com.cn/Article/CJFDTOTAL-DZKQ202002009.htm

    Li Z, Zhang Z Y, He D F, et al. Comparison in petroleum geology between Biyang Depression and Nanyang Depression in Nanxiang Basin and its exploration significance[J]. Bulletin of Geological Science and Technology, 2020, 39(2): 79-89(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-DZKQ202002009.htm
    [11] 刁慧, 邹玮, 李宁, 等. 东海盆地西湖凹陷武云亭构造油气来源与成藏模式[J]. 地质科技通报, 2020, 39(3): 110-119. https://www.cnki.com.cn/Article/CJFDTOTAL-DZKQ202003015.htm

    Diao H, Zou W, Li N, et al. Hydrocarbon origin and reservoir forming model of Wuyunting structure in Xihu Depression, East China Sea Basin[J]. Bulletin of Geological Science and Technology, 2020, 39(3): 110-119(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-DZKQ202003015.htm
    [12] 刘妍鷨, 陈红汉, 苏奥, 等. 从含油气检测来洞悉琼东南盆地东部发育始新统烃源岩的可能性[J]. 地球科学, 2016, 41(9): 1539-1547. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX201609009.htm

    Liu Y H, Chen H H, Su A, et al. Eocene source rock determination in Qiongdongnan Basin, the South China Sea: a hydrocarbon detection perspective[J]. Earth Science, 2016, 41(9): 1539-1547(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX201609009.htm
    [13] 任建业, 庞雄, 雷超, 等. 被动陆缘洋陆转换带和岩石圈伸展破裂过程分析及其对南海陆缘深水盆地研究的启示[J]. 地学前缘, 2015, 22(1): 102-114. https://www.cnki.com.cn/Article/CJFDTOTAL-DXQY201501011.htm

    Ren J Y, Pang X, Lei C, et al. Ocean and continent transition in passive continental margins and analysis of lithospheric extension and breakup process: Implication for research of the deepwater basins in the continental margins of South China Sea[J]. Earth Science Frontiers, 2015, 22(1): 102-114(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-DXQY201501011.htm
    [14] 米立军, 柳保军, 何敏, 等. 南海北部陆缘白云深水区油气地质特征与勘探方向[J]. 中国海上油气, 2016, 28(2): 10-12. https://www.cnki.com.cn/Article/CJFDTOTAL-ZHSD201602002.htm

    Mi L J, Liu B J, He M, et al. Petroleum geology characteristics and exploration direction in Baiyun deep water area, northern continental margin of the South China Sea[J]. China Offshore Oil and Gas, 2016, 28(2): 10-12(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-ZHSD201602002.htm
    [15] 李平鲁, 梁慧娴. 珠江口盆地新生代岩浆活动与盆地演化、油气聚集的关系[J]. 广东地质, 1994, 9(2): 23-24.

    Li P L, Liang H X. Relationship between Cenozoic magmatic activity and basin evolution and hydrocarbon accumulation in the Pearl River Mouth Basin[J]. Guangdong Geology, 1994, 9(2): 23-24(in Chinese with English abstract).
    [16] 倪金龙, 夏斌, 刘海龄. 南海及邻区前中生代构造演化与东特提斯构造域[J]. 海洋地质动态, 2005, 21(10): 11-16. https://www.cnki.com.cn/Article/CJFDTOTAL-HYDT200510002.htm

    Ni J L, Xia B, Liu H L. Pre-Mesozoic tectonic evolution of the South China Sea and the East Tethys tectonic domain[J]. Marine Geology Letters, 2005, 21(10): 11-16(in Chinese). https://www.cnki.com.cn/Article/CJFDTOTAL-HYDT200510002.htm
    [17] 张斌, 王璞珺, 张功成, 等. 珠-琼盆地新生界火山岩特征及其油气地质意义[J]. 石油勘探与开发, 2013, 40(6): 657-665. https://www.cnki.com.cn/Article/CJFDTOTAL-SKYK201306004.htm

    Zhang B, Wang P J, Zhang G C, et al. Cenozoic volcanic rocks in the Pearl River Mouth and Southeast Hainan Basins of South China Sea and their implications for petroleum geology[J]. Petroleum Exploration and Development, 2013, 40(6): 657-665(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-SKYK201306004.htm
    [18] 邵磊, 孟晓捷, 张功成, 等. 白云凹陷断裂特征对构造与沉积的控制作用[J]. 同济大学学报: 自然科学版, 2013, 41(9): 1435-1441. doi: 10.3969/j.issn.0253-374x.2013.09.025

    Shao L, Meng X J, Zhang G C, et al. Feature of faults system and its influence on tectonic and sedimentary history of Baiyun Sag[J]. Journal of Tongji University (Natural Science), 2013, 41(9): 1435-1441(in Chinese with English abstract). doi: 10.3969/j.issn.0253-374x.2013.09.025
    [19] Sun Q, Cartwright J, Wu S, et al. 3D seismic interpretation of dissolution pipes in the South China Sea: Genesis by subsurface, fluid induced collapse[J]. Marine Geology, 2013, 337(3): 171-181.
    [20] Lollar B S, O'Nions R K, Ballentine C J. Helium and neon isotope systematics in carbon dioxide-rich and hydrocarbon-rich gas reservoirs[J]. Geochimica et Cosmochimica Acta, 1994, 58(23): 5279-5290. doi: 10.1016/0016-7037(94)90311-5
    [21] Hulston J R, Hilton D R, Kaplan I R. Helium and carbon isotope systematics of natural gases from Taranaki Basin, New Zealand[J]. Applied Geochemistry, 2001, 16(4): 419-436. doi: 10.1016/S0883-2927(00)00045-7
    [22] Lupton J E. Terrestrial inert gases: Isotope tracer studies and clues to primordial components in the mantle[J]. Annual Review of Earth and Planetary Science Letters, 1983, 11(1): 371-414. doi: 10.1146/annurev.ea.11.050183.002103
    [23] Poreda R J, Jenden P D, Kaplan I R, et al. Mantle helium in Sacramento basin natural gas wells[J]. Geochimica et Cosmochimica Acta, 1986, 50(12): 2847-2853. doi: 10.1016/0016-7037(86)90231-0
    [24] Lollar B S, Ballentine C J, Onions R K. The fate of mantle-derived carbon in a continental sedimentary basin: Integration of C/He relationships and stable isotope signatures[J]. Geochimica et Cosmochimica Acta, 1997, 61(11): 2295-2307. doi: 10.1016/S0016-7037(97)00083-5
    [25] Huang B, Tian H, Huang H. Origin and accumulation of CO2 and its natural displacement of oils in the continental margin basins, northern South China Sea[J]. AAPG Bulletin, 2015, 99(7): 1349-1369. doi: 10.1306/02091514125
    [26] Li F, Li W. Petrological record of CO2 influx in the Dongying Sag, Bohai Bay Basin, NE China[J]. Applied Geochemistry. 2017, 84: 373-386. doi: 10.1016/j.apgeochem.2017.07.015
    [27] Zhao S, Liu L, Liu N. Petrographic and stable isotopic evidences of CO2-induced alterations in sandstones in the Lishui sag, East China Sea Basin, China[J]. Applied Geochemistry. 2018, 90: 115-128. doi: 10.1016/j.apgeochem.2018.01.004
    [28] 徐思萌. 含有孔虫泥质粉砂岩内片钠铝石纵向分布特征与成因[D]. 长春: 吉林大学, 2017.

    Xu S M. The vertical distribution characteristics and genesis of dawsonite in pelitic siltstone with foraminifers: a case studying in LWX well of the eastern South China Sea[D]. Changchun: Jilin University, 2017(in Chinese with English abstract).
    [29] Hellevang H, Declercq J, Aagaard P. Why is Dawsonite Absent in CO2 Charged Reservoirs?[J]. Oil & Gas Science & Technology, 2011, 66(1): 119-135.
    [30] Stoessell R K. Regular Solution Site-Mixing Model for Chlorites[J]. Clays and Clay Minerals, 1984, 32(3): 205-212. doi: 10.1346/CCMN.1984.0320308
  • 加载中
图(11) / 表(4)
计量
  • 文章访问数:  123
  • HTML全文浏览量:  30
  • PDF下载量:  569
  • 被引次数: 0
出版历程
  • 收稿日期:  2020-09-24

目录

    /

    返回文章
    返回