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琼东南盆地宝岛21-1区陵水组沉积特征及其油气地质意义

江汝锋 曹立成 邓孝亮 何云龙 焦垚祺 陈子归 李韬 张祺

江汝锋, 曹立成, 邓孝亮, 何云龙, 焦垚祺, 陈子归, 李韬, 张祺. 琼东南盆地宝岛21-1区陵水组沉积特征及其油气地质意义[J]. 地质科技通报, 2024, 43(5): 31-44. doi: 10.19509/j.cnki.dzkq.tb20230329
引用本文: 江汝锋, 曹立成, 邓孝亮, 何云龙, 焦垚祺, 陈子归, 李韬, 张祺. 琼东南盆地宝岛21-1区陵水组沉积特征及其油气地质意义[J]. 地质科技通报, 2024, 43(5): 31-44. doi: 10.19509/j.cnki.dzkq.tb20230329
JIANG Rufeng, CAO Licheng, DENG Xiaoliang, HE Yunlong, JIAO Yaoqi, CHEN Zigui, LI Tao, ZHANG Qi. Sedimentary characteristics of the Lingshui Formation in the Baodao 21-1 area of the Qiongdongnan Basin and their significance in hydrocarbon exploration[J]. Bulletin of Geological Science and Technology, 2024, 43(5): 31-44. doi: 10.19509/j.cnki.dzkq.tb20230329
Citation: JIANG Rufeng, CAO Licheng, DENG Xiaoliang, HE Yunlong, JIAO Yaoqi, CHEN Zigui, LI Tao, ZHANG Qi. Sedimentary characteristics of the Lingshui Formation in the Baodao 21-1 area of the Qiongdongnan Basin and their significance in hydrocarbon exploration[J]. Bulletin of Geological Science and Technology, 2024, 43(5): 31-44. doi: 10.19509/j.cnki.dzkq.tb20230329

琼东南盆地宝岛21-1区陵水组沉积特征及其油气地质意义

doi: 10.19509/j.cnki.dzkq.tb20230329
基金项目: 

中海石油(中国)有限公司科技项目课题 CCL2021HNFN0219

中央高校优秀青年团队项目"南海深水沉积过程及资源效应" 

详细信息
    作者简介:

    江汝锋, E-mail: jiangrf2@cnooc.com.cn

    通讯作者:

    曹立成,E-mail:lichengcao@cug.edu.cn

  • 中图分类号: P618. 130.2

Sedimentary characteristics of the Lingshui Formation in the Baodao 21-1 area of the Qiongdongnan Basin and their significance in hydrocarbon exploration

More Information
  • 摘要:

    近期在琼东南盆地宝岛21-1区发现了我国首个深水深层大气田, 对南海深水区深层油气勘探研究具有重要意义。基于宝岛21-1区最新获得的钻井和地震资料, 分析了上渐新统陵水组三段的沉积特征及其油气地质意义。结果表明, 陵三段沉积时期以双向物源为主, 早期扇三角洲沉积发育于邻近高地, 晚期辫状河三角洲沉积受NW向海南隆起物源和NE向神狐隆起物源的控制。此外, 陡坡和缓坡的沉积物搬运通道表现出较大差异。陵三段沉积演化可分为3个阶段: 由早期扇三角洲沉积、中期扇三角洲-辫状河三角洲沉积发展至晚期辫状河三角洲沉积, 物源区也从早期邻近高地的单向供源、中期邻近高地-神狐隆起的双向供源演化至晚期海南隆起-神狐隆起的双向供源。研究区邻近崖城组烃源岩, 发育12-1号断裂及伴生断裂, 形成构造-岩性圈闭, 成藏地质条件优越。宝岛21-1区气田的发现是我国深水油气勘探领域的重大突破, 指明了海相盆地中断裂转换带是未来深水勘探的关键区域。

     

  • 图 1  琼东南盆地构造单元图及研究区位置(修改自文献[2])

    Figure 1.  Tectonic units of the Qiongdongnan Basin and the study area location

    图 2  琼东南盆地地层柱状图(修改自文献[36])

    Figure 2.  Stratigraphic column of the Qiongdongnan Basin

    图 3  研究区层序地层剖面解释(a)及过A、B、C井陵三段连井剖面(b, c) (各地震界面代号见图 2,井位及剖面位置见图 1, 下同)

    MFS为最大洪泛面;GR为自然伽马曲线;DTCO为声波时差曲线

    Figure 3.  Sequence stratigraphic framework of the Third Member of the Lingshui Formation showing the seismic profile(a) and wells (wells A, B, and C)(b, c)

    图 4  宝岛21-1区D井陵三段岩性柱状图

    Figure 4.  Lithological column for the Third Member of the Lingshui Formation in Well D of the Baodao 21-1 area

    图 5  宝岛21-1区D井陵三段典型岩心照片

    Figure 5.  Typical core images of the Third Member of the Lingshui Formation in Well D of the Baodao 21-1 area

    图 6  宝岛21-1区过陵三段扇三角洲(a)及辫状河三角洲(b)地震剖面(井位及剖面位置见图 1, 地震界面代号见图 2)

    F12为宝岛凹陷12号断层; MFS为最大洪泛面

    Figure 6.  Seismic profiles showing the fan delta(a) and braided river delta(b) of the Third Member of the Lingshui Formation in the Baodao 21-1 Area

    图 7  基于地震均方根振幅与相干体切片(深度3 000 m)揭示的宝岛21-1区陵三段6期(a~f对应第1~6期) 砂体展布

    Figure 7.  Distributions of the six-phase sandstone bodies in the Third Member of the Lingshui Formation in the Baodao 21-1 area, revealed by the root mean square amplitude and coherence slice(3 000 m)

    图 8  研究区北部平行海南隆起物源方向地震剖面(地震界面代号见图 2,剖面位置见图 7f)

    Figure 8.  Seismic profile in the north of the study area striking parallel to the provenance direction of the Hainan Uplift

    图 9  研究区扇三角洲(a, b)和辫状河三角洲(c, d)沉积搬运方式(地震界面代号见图 2,剖面位置见图 7f)

    Figure 9.  Sediment transport types of fan delta (a, b) and braided river delta (c, d) in the study area

    图 10  宝岛21-1区陵三段沉积演化

    a, b, c.低位体系域第1, 2, 3期沉积体系展布; d, e, f.高位低系域第4, 5, 6期沉积体系展布

    Figure 10.  Sedimentary evolution of the Third Member of the Lingshui Formation in the Baodao 21-1 area

    图 11  宝岛21-1区地震剖面(a)及油气运移模式示意图(b) (地震界面代号见图 2,剖面位置见图 7f)

    Figure 11.  Seismic profile(a) and schematic model of petroleum migration(b) in the Baodao 21-1 area

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  • 收稿日期:  2023-06-09
  • 录用日期:  2023-11-01
  • 修回日期:  2023-10-30

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