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涠洲12-A油田流二段Ⅱ油组沉积特征及演化

曾小明,  张辉,  彭松,  周展,  王磊,  谢京

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文章导航 > 沉积学报  > 2015 >  33(1): 153-159
曾小明, 张辉, 彭松, 周展, 王磊, 谢京. 涠洲12-A油田流二段Ⅱ油组沉积特征及演化[J]. 沉积学报, 2015, 33(1): 153-159. doi: 10.14027/j.cnki.cjxb.2015.01.016
引用本文: 曾小明, 张辉, 彭松, 周展, 王磊, 谢京. 涠洲12-A油田流二段Ⅱ油组沉积特征及演化[J]. 沉积学报, 2015, 33(1): 153-159. doi: 10.14027/j.cnki.cjxb.2015.01.016
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ZENG XiaoMing, ZHANG Hui, PENG Song, ZHOU Zhan, WANG Lei, XIE Jing. Sedimentary Characteristics and Evolution of the 2nd Oil Series in the 2nd Member of Liushagang Formation in Weizhou12-A Oilfield[J]. Acta Sedimentologica Sinica, 2015, 33(1): 153-159. doi: 10.14027/j.cnki.cjxb.2015.01.016
Citation: ZENG XiaoMing, ZHANG Hui, PENG Song, ZHOU Zhan, WANG Lei, XIE Jing. Sedimentary Characteristics and Evolution of the 2nd Oil Series in the 2nd Member of Liushagang Formation in Weizhou12-A Oilfield[J]. Acta Sedimentologica Sinica, 2015, 33(1): 153-159. doi: 10.14027/j.cnki.cjxb.2015.01.016
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涠洲12-A油田流二段Ⅱ油组沉积特征及演化

doi: 10.14027/j.cnki.cjxb.2015.01.016
  • 1.

    中海石油(中国)有限公司湛江分公司 广东湛江 524057;

  • 2.

    中海石油(中国)有限公司天津分公司 天津 300452

详细信息
    作者简介:

    曾小明 男 1987年出生 硕士 助理工程师 储层预测和评价 E-mail:zengxm4@cnooc.com.cn

  • 中图分类号: P512.2

Sedimentary Characteristics and Evolution of the 2nd Oil Series in the 2nd Member of Liushagang Formation in Weizhou12-A Oilfield

  • 1.

    Zhanjiang Branch, CNOOC Ltd., Zhanjiang, Guangdong 524057;

  • 2.

    Tianjin Branch, CNOOC Ltd., Tianjin 300452

    摘要
  • 摘要: 北部湾盆地涠西南凹陷涠洲12-A油田流沙港组二段Ⅱ油组构造复杂,沉积差异大,横向变化快,对物源和沉积相的认识存在争议.通过测井、岩壁芯和地震等资料的分析研究,明确了涠洲12-A油田流沙港组二段Ⅱ油组物源来自于西南方向的涠洲12-8构造脊;划分了2长期基准面旋回、3个中期基准面旋回,建立了相应的等时层序格架;通过分析不同油组的沉积特征差异,识别出了两种沉积相,其中底部为扇三角洲沉积,顶部为正常三角洲沉积;并从基准面旋回的角度探讨了其沉积模式和演化规律.
    Abstract: The structure and sedimentary characteristics of the 2nd oil series in the 2nd Member of Liushagang Formation in Weizhou12-A oilfield, Weixinan depression, Beibu Gulf basin were very complex. Based on the analysis of the data of well logging, core and seismic data, it is obvious that the provenance of the 2nd oil series in the 2nd Member of Liushagang Formation in Weizhou12-A oilfield is from the southwest Weizhou 12-8 structure ridge; two long-term base level cycle and three medium-term base level cycles were divided, isochronous sequence stratigraphic framework was established; two sedimentary facies were identified by analyzing the differences of sedimentary characteristics of different oil group, the bottom of the 2nd oil series developed fan-delta depositional system, the top developed normal delta depositional system; the evolution sedimentary characteristics was discussed from the aspect of base level cycle.
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    • 参考文献(21)
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  • 收稿日期:  2014-02-15
  • 修回日期:  2014-04-09
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目录

    涠洲12-A油田流二段Ⅱ油组沉积特征及演化

    doi: 10.14027/j.cnki.cjxb.2015.01.016
    • 1. 中海石油(中国)有限公司湛江分公司 广东湛江 524057;
    • 2. 中海石油(中国)有限公司天津分公司 天津 300452
      • 作者简介:

      曾小明 男 1987年出生 硕士 助理工程师 储层预测和评价 E-mail:zengxm4@cnooc.com.cn

    • 收稿日期: 2014-02-15
    • 修回日期: 2014-04-09
    • 刊出日期: 2015-02-10

    • 中图分类号: P512.2

    摘要: 北部湾盆地涠西南凹陷涠洲12-A油田流沙港组二段Ⅱ油组构造复杂,沉积差异大,横向变化快,对物源和沉积相的认识存在争议.通过测井、岩壁芯和地震等资料的分析研究,明确了涠洲12-A油田流沙港组二段Ⅱ油组物源来自于西南方向的涠洲12-8构造脊;划分了2长期基准面旋回、3个中期基准面旋回,建立了相应的等时层序格架;通过分析不同油组的沉积特征差异,识别出了两种沉积相,其中底部为扇三角洲沉积,顶部为正常三角洲沉积;并从基准面旋回的角度探讨了其沉积模式和演化规律.

    English Abstract

    曾小明, 张辉, 彭松, 周展, 王磊, 谢京. 涠洲12-A油田流二段Ⅱ油组沉积特征及演化[J]. 沉积学报, 2015, 33(1): 153-159. doi: 10.14027/j.cnki.cjxb.2015.01.016
    引用本文: 曾小明, 张辉, 彭松, 周展, 王磊, 谢京. 涠洲12-A油田流二段Ⅱ油组沉积特征及演化[J]. 沉积学报, 2015, 33(1): 153-159. doi: 10.14027/j.cnki.cjxb.2015.01.016
    shu
    ZENG XiaoMing, ZHANG Hui, PENG Song, ZHOU Zhan, WANG Lei, XIE Jing. Sedimentary Characteristics and Evolution of the 2nd Oil Series in the 2nd Member of Liushagang Formation in Weizhou12-A Oilfield[J]. Acta Sedimentologica Sinica, 2015, 33(1): 153-159. doi: 10.14027/j.cnki.cjxb.2015.01.016
    Citation: ZENG XiaoMing, ZHANG Hui, PENG Song, ZHOU Zhan, WANG Lei, XIE Jing. Sedimentary Characteristics and Evolution of the 2nd Oil Series in the 2nd Member of Liushagang Formation in Weizhou12-A Oilfield[J]. Acta Sedimentologica Sinica, 2015, 33(1): 153-159. doi: 10.14027/j.cnki.cjxb.2015.01.016
    shu

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