• 中国出版政府奖提名奖

    中国百强科技报刊

    湖北出版政府奖

    中国高校百佳科技期刊

    中国最美期刊

    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

    琼东南盆地宝岛-长昌凹陷陵水组储层差异演化特征

    钟佳 杨希冰 朱沛苑 徐守立 邓孝亮 庹雷 李兴 宋鹏

    钟佳, 杨希冰, 朱沛苑, 徐守立, 邓孝亮, 庹雷, 李兴, 宋鹏, 2019. 琼东南盆地宝岛-长昌凹陷陵水组储层差异演化特征. 地球科学, 44(8): 2665-2676. doi: 10.3799/dqkx.2019.097
    引用本文: 钟佳, 杨希冰, 朱沛苑, 徐守立, 邓孝亮, 庹雷, 李兴, 宋鹏, 2019. 琼东南盆地宝岛-长昌凹陷陵水组储层差异演化特征. 地球科学, 44(8): 2665-2676. doi: 10.3799/dqkx.2019.097
    Zhong Jia, Yang Xibing, Zhu Peiyuan, Xu Shouli, Deng Xiaoliang, Tuo Lei, Li Xing, Song Peng, 2019. Porosity Evolution Differences of the Lingshui Formation Reservoir between Baodao and Changchang Sag, Qiongdongnan Basin. Earth Science, 44(8): 2665-2676. doi: 10.3799/dqkx.2019.097
    Citation: Zhong Jia, Yang Xibing, Zhu Peiyuan, Xu Shouli, Deng Xiaoliang, Tuo Lei, Li Xing, Song Peng, 2019. Porosity Evolution Differences of the Lingshui Formation Reservoir between Baodao and Changchang Sag, Qiongdongnan Basin. Earth Science, 44(8): 2665-2676. doi: 10.3799/dqkx.2019.097

    琼东南盆地宝岛-长昌凹陷陵水组储层差异演化特征

    doi: 10.3799/dqkx.2019.097
    基金项目: 

    国家科技重大专项 2016ZX05026-002

    中海石油(中国)有限公司自主立项项目 ZYKY-2018-ZJ-01

    详细信息
      作者简介:

      钟佳(1987-), 男, 工程师, 硕士, 主要从事沉积储层研究

    • 中图分类号: P618

    Porosity Evolution Differences of the Lingshui Formation Reservoir between Baodao and Changchang Sag, Qiongdongnan Basin

    • 摘要: 宝岛-长昌凹陷陵水组砂岩储集体目前是琼东南盆地油气勘探的重点目标.本文综合铸体薄片、激光粒度、元素地球化学、X衍射、扫描电镜、流体包裹体以及电子探针分析,探究宝岛凹陷北坡与长昌凹陷陵水组砂岩储层的成岩演化差异性.宝岛凹陷北坡的砂岩储层具有“粒度粗、稳定组分高”的强水动力特征,是海南岛物源体系下的三角洲沉积;而长昌凹陷砂岩储层具有“粒级偏细、泥质杂基重”的弱水动力特点,是神狐隆起、西沙隆起物源体系下的海底扇沉积.机械压实导致宝岛凹陷北坡的陵水组砂岩储层颗粒普遍呈现线状或凹凸接触.高热流背景导致长昌凹陷陵水组砂岩在海底以下浅埋条件(海底以下约1 400 m)下即可进入化学压实阶段,颗粒呈点-线接触,并伴生重晶石、片钠铝石等热液矿物.宝岛凹陷北坡存在早、晚两期烃类充注(14.5~10.0 Ma、2~0 Ma),期间被一期CO2充注分隔(7~3 Ma).长昌凹陷仅发育早期烃类充注(14.5~6.0 Ma),以及随后的一期CO2充注(5~0 Ma).陵水组砂岩储层演化在宝岛凹陷北坡总体以“海底以下缓慢深埋、缓慢升温”,天然气充注促进溶蚀和抑制胶结为特点,而长昌凹陷则以“海底以下浅埋、快速升温”,CO2持续充注促使碳酸盐或粘土或热液矿物胶结为特点.

       

    • 图  1  宝岛-长昌凹陷陵水组储集体分布与连井沉积相剖面

      Fig.  1.  The distribution and wells section of sedimentary facies of Lingshui formation reservior in Baodao-Changchang sag

      图  2  长昌凹陷陵水组与神狐隆起区稀土元素石标准化配分模式

      Fig.  2.  The chondrite-normalized REE pattern of Lingshui formation in Changchang sag and rocks in Shenhu uplift

      图  3  宝岛-长昌凹陷陵水组砂岩岩石类型

      Fig.  3.  Sandstone composition classification of Lingshui formation reservoir in Baodao-Changchang sag

      图  4  宝岛-长昌凹陷陵水组储层粒度C-M与典型粒度概率曲线

      Fig.  4.  C-M patterns and typical probability cumulative curves of Lingshui Formation Reservoir in Baodao-Changchang Sag

      图  5  宝岛-长昌区成岩阶段对比及对应莫霍面埋深

      Fig.  5.  The digenetic stage contrast and corresponding Moho surface depth in Baodao-Changchang area

      图  6  宝岛-长昌区陵水组储层成岩作用类型显微照片

      a.B-3, 4 104.5 m, 中-粗砂岩, 颗粒呈线接触, 石英次生加大, 壁心(-);b.W-1, 4 855.5 m, 细砂岩, 颗粒呈点-线接触, 石英次生加大, 壁心(-);c.B-3, 4 104.5 m, 中-粗砂岩, 长石与岩屑颗粒溶蚀, 壁心(-);d.W-1, 4 855.5 m, 细砂岩, 长石颗粒溶蚀、片丝状伊利石充填粒间, 扫描电镜, 壁心;e.B-3, 3 936.0 m, 中-粗砂岩, 片丝状伊利石充填颗粒之间, 扫描电镜, 壁心;f.B-3, 4 102.0 m, 中-粗砂岩, 连晶铁方解石胶结与铁白云石交代, 壁心(-);g.W-1, 4 920.0 m, 极细砂岩, 电子探针片, 背散射成像, 壁心;h.探针点1:重晶石, 探针点2:铁白云石;i.C-1, 3 360.8 m, 极细砂岩, 放射状片钠铝石, 壁心(-)

      Fig.  6.  Microphotographs showing digenesis of Lingshui Formation Reservoir in Baodao-Changchang area

      图  7  宝岛-长昌凹陷典型陵水组储层盐水包裹体均一温度及埋藏史

      Fig.  7.  The homogenization temperature of aqueous inclusions in typical Lingshui Formation Reservoir in Baodao-Changchang Sag and burial history

      图  8  宝岛凹陷北坡与长昌凹陷陵水组储层成岩-孔隙差异演化模式

      Fig.  8.  Variations in digenesis and pore evolution of Lingshui formation reservoir between Baodao sag′s Northern slope and Changchang sag

      表  1  宝岛-长昌凹陷陵水组储层岩石组分特征

      Table  1.   Parameters of sandstone components of Lingshui Formation Reservior in Baodao-Changchang Sag

      井号 粒度 砂体类型 岩石类型 单晶石英(%) 长石(%) 岩屑(%) 碳酸盐胶结物(%) 泥质杂基(%) 黏土矿物含量(%)
      多晶石英 花岗岩 变质岩 喷出岩 沉积岩 云母 伊利石 高岭石 绿泥石 伊蒙混层
      A-1 中、粗 三角洲 岩屑石英砂岩、长石岩屑砂岩 51.3 7.2 16.3 0.2 3.7 1.0 0 0.2 3.7 6.7
      D-1 48.5 9.9 15.0 0.6 4.2 1.0 0 0.3 6.3 3.3
      B-3 54.8 8.8 12.8 0.1 6.5 2.5 0 0.1 7.3 4.4 64.9 4.9 4.5 25.7
      W-1 粉、细 海底扇 岩屑石英砂岩 51.5 6.8 8.2 0 6.6 0.8 0 0.5 6.2 12.5 76.9 4.1 0.9 18.1
      下载: 导出CSV
    • Cai, J., 2017. Sedimentary Facies of Neogene Sanya Formation in Changchang Sag, Qiongdongnan Basin. Lithologic Reservoirs, 29(5):46-54(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=yxyqc201705006
      Cai, J., Wang, H., 2011. The Temporal and Spatial Configure Relation of Sedimentary Systems and Sequence Stratigraphic Framework of Lingshui Formation in Qiongdongnan Basin. Offshore Oil, 31(1):16-21(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=hysy201101003
      Cao, L.C., 2014. Provenance Evolution since Neogene in the Yinggehai and Qiongdongnan Basins: Evidence from REE, Heavy Mineral and Ziron U-Pb Ages(Dissertation). China University of Geosciences, Wuhan (in Chinese with English abstract).
      Fischer, C., Dunkl, I., von Eynatten, H., et al., 2012. Products and Timing of Diagenetic Processes in Upper Rotliegend Sandstones from Bebertal (North German Basin, Parchim Formation, Flechtingen High, Germany). Geological Magazine, 149(5): 827-840. https://doi.org/10.1017/s0016756811001087
      Fitch, P. J. R., Lovell, M. A., Davies, S. J., et al., 2015. An Integrated and Quantitative Approach to Petrophysical Heterogeneity. Marine and Petroleum Geology, 63: 82-96. https://doi.org/10.13039/501100000270
      Gao, Y.Q., Liu, L., Qu, X.Y., 2005. Gemesis of Dawsonite and Its Indication Significance of CO2 Migration and Accumulation. Advances in Earth Science, 20(10): 1083-1088(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dqkxjz200510006
      Gong, Z.S., Li, S.T., Xie, Q.J., 1997. Continental Margin Basin Analysis and Hydrocarbon Accumulation of the Northern South China Sea. Science Press, Beijing (in Chinese).
      Li, C., Chen, G.J., Zhang, G. C., et al., 2017. Developmental Characteristics and Provenances of the Submarine Fans Developed during the Middle Miocene in the Eastern Deepwater Area of the Qiongdongnan Basin. Natural Gas Geoscience, 28(10):1555-1564(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=trqdqkx201710010
      Li, C., Luo, J.L., Hu, H.Y., et al., 2018. The Thermodynamic Impact on Deepwater Sandstone Diagenetic Evolution of the Zhuhai Formation in Baiyun Sag, Pearl River Mouth Basin. Earth Science, 44(2):572-583(in Chinese with English abstract).
      Li, C., Luo, X.R., 2017. Review on Mudstone Chemical Compaction. Journal of Earth Sciences & Environment, 39(6): 761-772(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=xagcxyxb201706007
      Li, X.X., 2004.Study on Structural Dynamics and Hydrocarbon Accumulation in Qiongdongnan Basin(Dissertation). Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou (in Chinese with English abstract).
      Li, Z.X., Song, G.Z., Wang, D.D., et al., 2018. Characteristics of (Fan) Braided River Delta in Oligocene Coal Measures of Qiongdongnan Basin. Earth Science, 43(10) : 3471-3484(in Chinese with English abstract). http://d.old.wanfangdata.com.cn/Periodical/dqkx201810011
      Liu, Y. H., Chen, H.H., Su, A., et al., 2016. Eocene Source Rock Determination in Qiongdongnan Basin, the South China Sea: A Hydrocarbon Detection Perspective. Earth Science, 41(9): 1539-1547(in Chinese with English abstract). http://d.old.wanfangdata.com.cn/Periodical/dqkx201609009
      Liu, Z. H., Chen, H.H., 2011.Hydrocarbon Charging Orders and Times in the Eastern Area of Qiongdongnan Basin. Geoscience, 25(2):279-288(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=xddz201102011
      Luo, J.L., Li, X. S., Fu, X.Y., et al., 2014.Impact of Petrologic Components and Their Diagenetic Evolution on Tight Sandstone Reservoir Quality and Gas Yield: A Case Study from He 8 Gas-Bearing Reservoir of Upper Paleozoic in Northern Ordos Basin. Earth Science, 39(5):537-545(in Chinese with English abstract). http://d.old.wanfangdata.com.cn/Periodical/dqkx201405004
      Mi, L. J., Yuan, Y.S., Zhang, G. C., et al., 2009. Characteristics and Genesis of Geothermal Field in Deep Water Area of the Northern South China Sea. Acta Petrolei Sinica, 30(1): 27-32(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-SYXB200901006.htm
      Schneider, F., Potdevin, J. L., Wolf, S., et al., 1996. Mechanical and Chemical Compaction Model for Sedimentary Basin Simulators. Tectonophysics, 263(1/2/3/4): 307-317. https://doi.org/10.1016/s0040-1951(96)00027-3
      Shao, L., Cao, L. C., Pang, X., et al., 2016. Detrital Zircon Provenance of the Paleogene Syn-Rift Sediments in the Northern South China Sea. Geochemistry, Geophysics, Geosystems, 17(2): 255-269. https://doi.org/10.13039/501100001809
      Shao, L., Li, A., Wu, G.X., et al., 2010. Evolution of Sedimentary Environment and Provenance in Qiongdongnan Basin in the Northern South China Sea. Acta Petrolei Sinica, 31(4): 548-552(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=syxb201004005
      Song, G. Z., Wang, H., Gan, H. J., et al., 2014. Paleogene Tectonic Evolution Controls on Sequence Stratigraphic Patterns in the Central Part of Deepwater Area of Qiongdongnan Basin, Northern South China Sea. Journal of Earth Science, 25(2): 275-288. https://doi.org/10.1007/s12583-014-0433-7
      Wang, C., Liang, X.Q., Tong, C.X., et al., 2014. Characteristics and Geological Implications of Heavy Minerals from Seven Rivers in Adjacent Areas of Northeastern Yinggehai Basin. Acta Sedimentologica Sinica, 32(2): 228-237 (in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=cjxb201402005
      Wu, J.F., Yang, S.C., Zhang, G. C., et al., 2016. Geothermal History and Thermal Evolution of the Source Rocks in the Deep-Water Area of the Northern South China Sea. Chinese Journal of Geophysics, 56(1): 170-180(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dqwlxb201301017
      Xie, Y.H., 2014. A Major Breakthrough in Deepwater Natural Gas Exploration in Self-Run Oil/Gas Field in the Northern South China Sea and Its Enlightenment. Natural Gas Industry, 34(10): 1-8 (in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=trqgy201410001
      Ying, F.X., He, D.B., Long, Y.M., et al., 2003. SY/T5477-2003 the Industry Standard of China and Division of Diagenetic Stage s in Clastic Rocks(Standard). Petroleum Industry Press, Beijing (in Chinese).
      Zhang, G. C., Zhang, Y.N., Shen, H.L., et al., 2014. An Analysis of Natural Gas Exploration Potential in the Qiongdongnan Basin by Use of the Theory of Joint Control of Source Rocks and Geothermal Heat. Natural Gas Industry, 34(1):18-27(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=Doaj000004076749
      Zhang, Y.X., Zhu, X.M., Zhang, G.C., et al., 2013. Sedimentary Characteristics of Oligocene Lingshui Formation in Qiongdongnan Basin, South China Sea. Natural Gas Geoscience, 24(5):956-964(in Chinese with English abstract). http://d.old.wanfangdata.com.cn/Periodical/gdlxb201403008
      Zhang, Y.Z., Gan, J., Yang, X.B., et al., 2017a. Tectonic Evolution and Its Constraints on the Formation of Deepwater Giant Gas Field in Lingshui Sag, Qiongdongnan Basin. Marine Geology Frontiers, 33(10):22-31(in Chinese with English abstract). http://d.old.wanfangdata.com.cn/Periodical/hydzdt201710003
      Zhang, Y.Z., Xu, X.D., Gan, J., et al., 2017b. Study on the Geological Characteristics, Accumulation Model and Exploration Direction of the Giant Deepwater Gas Field in the Qiongdongnan Basin. Acta Geologica Sinica, 91(7):1620-1633(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dizhixb201707013
      Zhao, D.N., Zhu, X.M., Lin, J.C., et al., 2014. Sedimentary Characteristics and Evolution of Transitional Belt of the Paleogene Lingshui Formation in Ya13-1 Gasfield of Qiongdongnan Basin, South China Sea. Journal of Palaeogeography, 16(3):385-400 (in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=gdlxb201403008
      蔡佳, 2017.琼东南盆地长昌凹陷新近系三亚组沉积相.岩性油气藏, 29(5): 46-54. doi: 10.3969/j.issn.1673-8926.2017.05.006
      蔡佳, 王华, 2011.琼东南盆地陵水组层序地层格架及沉积体系的时空配置关系.海洋石油, 31(1):16-21. doi: 10.3969/j.issn.1008-2336.2011.01.016
      曹立成, 2014.莺歌海-琼东南盆地区新近纪物源演化研究(硕士学位论文).武汉: 中国地质大学. http://cdmd.cnki.com.cn/Article/CDMD-10491-1014340936.htm
      高玉巧, 刘立, 曲希玉, 2005.片钠铝石的成因及其对CO2天然气运聚的指示意义.地球科学进展, 20(10):1083-1088. doi: 10.3321/j.issn:1001-8166.2005.10.006
      龚再升, 李思田, 谢秦俊, 1997.南海北部大陆边缘盆地分析与油气聚集.北京:科学出版社.
      李超, 陈国俊, 张功成, 等, 2017.琼东南盆地深水区东段中中新世深水扇发育特征及物源分析.天然气地球科学, 28(10):1555-1564. http://d.old.wanfangdata.com.cn/Periodical/trqdqkx201710010
      李超, 罗晓容, 2017.泥岩化学压实作用研究进展.地球科学与环境学报, 39(6): 761-772. doi: 10.3969/j.issn.1672-6561.2017.06.007
      李弛, 罗静兰, 胡海燕, 等, 2018.热动力条件对白云凹陷深水区珠海组砂岩成岩演化过程的影响.地球科学, 44(2):572-583. http://www.earth-science.net/WebPage/Article.aspx?id=4133
      李绪宣, 2004.琼东南盆地构造动力学演化及油气成藏研究(博士学位论文).广州: 中国科学院研究生院(广州地球化学研究所). http://cdmd.cnki.com.cn/Article/CDMD-80165-2004108887.htm
      李增学, 宋广增, 王东东, 等, 2018.琼东南盆地渐新统煤系(扇)辫状河三角洲特征.地球科学, 43(10) : 3471-3484. http://www.earth-science.net/WebPage/Article.aspx?id=3990
      刘妍鷨, 陈红汉, 苏奥, 等, 2016.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.地球科学, 41(9): 1539-1547. http://www.earth-science.net/WebPage/Article.aspx?id=3359
      刘正华, 陈红汉, 2011.琼东南盆地东部地区油气形成期次和时期.现代地质, 25(2):279-288. doi: 10.3969/j.issn.1000-8527.2011.02.011
      罗静兰, 刘新社, 付晓燕, 等, 2014.岩石学组成及其成岩演化过程对致密砂岩储集质量与产能的影响:以鄂尔多斯盆地上古生界盒8天然气储层为例.地球科学, 39(5):537-545. http://www.earth-science.net/WebPage/Article.aspx?id=2862
      米立军, 袁玉松, 张功成, 等, 2009.南海北部深水区地热特征及其成因.石油学报, 30(1): 27-32. doi: 10.3321/j.issn:0253-2697.2009.01.005
      邵磊, 李昂, 吴国瑄, 等, 2010.琼东南盆地沉积环境及物源演变特征.石油学报, 31(4): 548-552. http://d.old.wanfangdata.com.cn/Periodical/syxb201004005
      王策, 梁新权, 童传新, 等, 2014.莺歌海盆地东北部邻区7条主要入海河流重砂矿物特征及其地质意义.沉积学报, 32(2): 228-237. http://d.old.wanfangdata.com.cn/Periodical/cjxb201402005
      吴景富, 杨树春, 张功成, 等, 2013.南海北部深水区盆地热历史及气源岩热演化研究.地球物理学报, 56(1): 170-180.
      谢玉洪, 2014.南海北部自营深水天然气勘探重大突破及其启示.天然气工业, 34(10): 1-8. doi: 10.3787/j.issn.1000-0976.2014.10.001
      应凤祥, 何东博, 龙玉梅, 等, 2003. SY/T5477-2003中华人民共和国石油天然气行业标准:碎屑岩成岩阶段划分.北京:石油工业出版社.
      张功成, 张义娜, 沈怀磊, 等, 2014. "源热共控"琼东南盆地的天然气勘探潜力.天然气工业, 34(1):18-27. doi: 10.3787/j.issn.1000-0976.2014.01.003
      张亚雄, 朱筱敏, 张功成, 等, 2013.中国南海琼东南盆地渐新统陵水组沉积特征.天然气地球科学, 24(5) :956-964. http://d.old.wanfangdata.com.cn/Periodical/trqdqkx201305011
      张迎朝, 甘军, 杨希冰, 等, 2017a.琼东南盆地陵水凹陷构造演化及其对深水大气田形成的控制作用.海洋地质前沿, 33(10):22-31. http://d.old.wanfangdata.com.cn/Periodical/hydzdt201710003
      张迎朝, 徐新德, 甘军, 等, 2017b.琼东南盆地深水大气田地质特征、成藏模式及勘探方向.地质学报, 91(7): 1620-1633. http://d.old.wanfangdata.com.cn/Periodical/dizhixb201707013
      赵东娜, 朱筱敏, 林金成, 等, 2014.南海琼东南盆地崖13-1气田古近系陵水组海陆过渡带沉积特征及演化.古地理学报, 16(3):385-400. http://d.old.wanfangdata.com.cn/Periodical/gdlxb201403008
    • 加载中
    图(8) / 表(1)
    计量
    • 文章访问数:  5457
    • HTML全文浏览量:  2560
    • PDF下载量:  56
    • 被引次数: 0
    出版历程
    • 收稿日期:  2019-01-23
    • 刊出日期:  2019-08-15

    目录

      /

      返回文章
      返回