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    琼东南盆地松南低凸起古近系构造-沉积演化特征与天然气成藏

    周杰 杨希冰 杨金海 甘军 吴昊 何小胡 胡斌

    周杰, 杨希冰, 杨金海, 甘军, 吴昊, 何小胡, 胡斌, 2019. 琼东南盆地松南低凸起古近系构造-沉积演化特征与天然气成藏. 地球科学, 44(8): 2704-2716. doi: 10.3799/dqkx.2019.104
    引用本文: 周杰, 杨希冰, 杨金海, 甘军, 吴昊, 何小胡, 胡斌, 2019. 琼东南盆地松南低凸起古近系构造-沉积演化特征与天然气成藏. 地球科学, 44(8): 2704-2716. doi: 10.3799/dqkx.2019.104
    Zhou Jie, Yang Xibing, Yang Jinhai, Gan Jun, Wu Hao, He Xiaohu, Hu Bin, 2019. Structure-Sedimentary Evolution and Gas Accumulation of Paleogene in Songnan Low Uplift of the Qiongdongnan Basin. Earth Science, 44(8): 2704-2716. doi: 10.3799/dqkx.2019.104
    Citation: Zhou Jie, Yang Xibing, Yang Jinhai, Gan Jun, Wu Hao, He Xiaohu, Hu Bin, 2019. Structure-Sedimentary Evolution and Gas Accumulation of Paleogene in Songnan Low Uplift of the Qiongdongnan Basin. Earth Science, 44(8): 2704-2716. doi: 10.3799/dqkx.2019.104

    琼东南盆地松南低凸起古近系构造-沉积演化特征与天然气成藏

    doi: 10.3799/dqkx.2019.104
    基金项目: 

    国家科技重大专项:琼东南盆地深水区大中型气田形成条件及勘探关键技术 2016ZX05026-002

    详细信息
      作者简介:

      周杰(1988-), 男, 工程师, 主要从事南海西部油气勘探研究工作

    • 中图分类号: P588

    Structure-Sedimentary Evolution and Gas Accumulation of Paleogene in Songnan Low Uplift of the Qiongdongnan Basin

    • 摘要: 为了明确松南低凸起区构造沉积演化特征及对天然气成藏的意义.基于区域长剖面精细解释,利用最新的钻井、测井、地震资料,分析了松南低凸起及围区古近系构造格局、斜坡类型及演化特征、沉积特征及与天然气成藏的关系.结果表明,松南低凸起主要受北部2号、12号断裂,南部11号、10号断裂活动控制,古近纪经历了:“(1)差异翘倾抬升,西高东低;(2)加速翘倾抬升,向东抬升”这2个阶段,并以发育旋转掀斜斜坡为主.古地貌具有“隆凹相间”与“西高东低”的特征.断裂活动及翘倾抬升作用控制了物源区的分布、缓坡沉积格局及输砂通道,在东突起上发育了缓坡带扇三角洲沉积.大面积分布的扇三角洲发育了优质的储集体,构造活动形成了多种类型的圈闭,天然气生、运、聚时空匹配良好,松南低凸起古近系有望成为琼东南盆地下一个千亿方级的天然气聚集区.

       

    • 图  1  琼东南盆地构造纲要

      Fig.  1.  Tectonic framework of the Qiongdong Basin showing the study area, seismic dataset, faults

      图  2  琼东南盆地地层综合柱状图

      Fig.  2.  Comprehensive stratigraphic column of the Qiongdongnan Basin

      图  3  研究区典型区域大剖面(剖面位置见图 1

      Fig.  3.  Typical seismic profile of studying area

      图  4  研究区斜坡类型

      Fig.  4.  Types of slopes in the study area

      图  5  始新统-陵水组沉积厚度图与2号11号断裂叠合图

      Fig.  5.  Overlaping map of thickness of Eocene-Lingshui formation, NO.2 and NO.11 faults activity rate

      图  6  松南低凸起早渐新世晚期崖城组古地貌图与典型地震剖面

      Fig.  6.  Paleogeomorphologic map and typical seismic profile of the Yacheng formation in the late Early Oligocene of Songnan low uplift

      图  7  Y-1井崖城组扇三角洲岩电特征

      Fig.  7.  Fan delta rock and log characteristics of Yacheng formation, Y-1

      图  8  过松南低凸起扇三角洲典型地震剖面(剖面位置见图 1)

      Fig.  8.  Typical seismic profile off an delta in the Songnan Low Uplift

      图  9  松南低凸起崖城组-陵水组沉积相

      Fig.  9.  Sedimentary facies map of Yacheng formation and Lingshui formation of the Songnan low uplift

      图  10  断层差异旋转翘倾缓坡带控三角洲沉积模式

      Fig.  10.  Deltaic sedimentation model controlled by fault differential rotation tilting gentle slope zone

      图  11  松南低凸起古近系天然气成藏模式

      Fig.  11.  Gas accumulation mode of Songnan Low Uplift in Qingdongnan Basin

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    • 收稿日期:  2019-01-21
    • 刊出日期:  2019-08-15

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