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    四川盆地震旦纪-早寒武世构造-沉积演化过程

    段金宝 梅庆华 李毕松 梁子锐

    段金宝, 梅庆华, 李毕松, 梁子锐, 2019. 四川盆地震旦纪-早寒武世构造-沉积演化过程. 地球科学, 44(3): 738-755. doi: 10.3799/dqkx.2018.335
    引用本文: 段金宝, 梅庆华, 李毕松, 梁子锐, 2019. 四川盆地震旦纪-早寒武世构造-沉积演化过程. 地球科学, 44(3): 738-755. doi: 10.3799/dqkx.2018.335
    Duan jinbao, Mei qinghua, Li bisong, Liang zirui, 2019. Sinian-Early Cambrian Tectonic-Sedimentary Evolution in Sichuan Basin. Earth Science, 44(3): 738-755. doi: 10.3799/dqkx.2018.335
    Citation: Duan jinbao, Mei qinghua, Li bisong, Liang zirui, 2019. Sinian-Early Cambrian Tectonic-Sedimentary Evolution in Sichuan Basin. Earth Science, 44(3): 738-755. doi: 10.3799/dqkx.2018.335

    四川盆地震旦纪-早寒武世构造-沉积演化过程

    doi: 10.3799/dqkx.2018.335
    基金项目: 

    国家自然科学基金重点项目 U1663210

    国家科技重大专项 2017ZX05005003

    详细信息
      作者简介:

      段金宝(1981-), 男, 研究员, 从事油气地质综合研究工作

    • 中图分类号: P618.13

    Sinian-Early Cambrian Tectonic-Sedimentary Evolution in Sichuan Basin

    • 摘要: 前人对四川盆地震旦纪-早寒武世构造-沉积演化的认识存在较大分歧.利用最新的地震、钻井及露头资料,系统论述了四川盆地震旦纪-早寒武世构造-沉积演化特征.四川盆地在陡山沱组沉积前呈现隆坳相间地貌格局,汉南古陆构造高点从陡山沱期到早寒武世持续向北东方向迁移;开江-宣汉古隆起灯一、灯二段沉积期为主要发育时期,古隆起核部出露水面,灯三、灯四段沉积期古隆起规模减小,转为水下隆起,到早寒武世与川中古隆起合并.通过连井剖面、典型井元素测井、野外露头特征综合分析认为德阳-安岳古裂陷槽内发育灯三、灯四段深水沉积.在此基础上总结古裂陷发育模式:古裂陷具有明显的多期发育特征,东侧台地边缘不断向北东方向迁移,灯二段沉积期台缘位于双探地区,灯四段沉积期台缘位于元坝西地区;同时古裂陷具有"北早南晚、先断陷后坳陷"的发育特征,灯影组沉积期在川中-川北发育,具有断陷发育特征,早寒武世裂陷槽转为坳陷发育特征,川南地区开始大规模发育,川中-川北地区持续向北东方向迁移,川北元坝-仁和场-马路背地区转化为深水沉积,发育厚层筇竹寺组烃源岩层系,至早寒武世晚期,古裂陷消亡、被填平补齐.

       

    • 图  1  四川盆地震旦系沉积前的古构造格局

      杨跃明等(2016)修改

      Fig.  1.  Paleostructural pattern before Sinian deposition in Sichuan Basin

      图  2  四川盆地川中-川北地区陡山沱组地层对比

      文龙(2016)杨跃明(2016)修改

      Fig.  2.  Stratigraphic correlation of Doushantuo Formation in central Sichuan and northern Sichuan

      图  3  德阳-安岳古裂陷两侧灯影组与麦地坪组地层对比

      李双建(2018)修改

      Fig.  3.  Stratigraphic correlation between the Dengying Formation and the Maidiping Formation on both sides of Deyang-Anyue ancient rift

      图  4  ZY1井震旦系-下寒武统元素测井柱状图

      李双建等(2018)修改

      Fig.  4.  Sinian-Lower Cambrian element log histogram of Well ZY1

      图  5  德阳-安岳古裂陷槽内灯影组沉积记录

      a.平武金凤剖面,灯影组和下寒武统邱家河组整体面貌;b.平武金凤剖面,灯影组薄层硅质岩和白云岩与邱家河组薄层白云岩呈不整合接触,但灯影组顶部未见溶孔和岩溶角砾;c.绵阳清平剖面,灯影组顶部中层状灰色细晶白云岩与薄层深灰色硅质岩、硅化白云岩互层;d.广元东溪河剖面,灯影组顶部的硅质碎屑岩,代表了斜坡相的硅质碎屑流,证实了斜坡的存在

      Fig.  5.  Sedimentary record of the Dengying Formation in the Deyang-Anyue ancient rift

      图  6  四川盆地龙王庙组-沧浪铺组地层对比

      Fig.  6.  Stratigraphic correlation of Longwangmiao and Canglangpu formations in Sichuan Basin

      图  7  通江三维地震剖面特征

      剖面位置见图 1

      Fig.  7.  The characteristics of Tongjiang 3D seismic profiles

      图  8  四川盆地灯影组不同时期地层厚度图(a)及古地貌图(b)

      Fig.  8.  Stratigraphic thickness map (a) and paleogeomorphic map (b) of Dengying Formation in Sichuan Basin at different periods

      图  9  川北典型二维地震剖面古裂陷特征

      灯影组底拉平,剖面位置见图 8AA

      Fig.  9.  The ancient rift characteristics in typical 2D seismic profile in North Sichuan

      图  10  川北地区灯影组地层对比

      Fig.  10.  Stratigraphic correlation of Dengying Formation in North Sichuan

      图  11  四川盆地麦地坪组-沧浪铺组地层厚度图(a)和古地貌图(b)

      Fig.  11.  Stratigraphic thickness map (a) and paleogeomorphic map (b) of Maidiping and Canglangpu formations in Sichuan Basin

      图  12  四川盆地龙王庙组地层厚度图

      Fig.  12.  The stratigraphic thickness map of Longwangmiao Formation in Sichuan Basin

      图  13  川中-川南地区灯影组地层对比

      Fig.  13.  Stratigraphic correlation of the Dengying Formation in central Sichuan and southern Sichuan

      图  14  川南灯影组典型二维地震剖面

      资阳-威远-泸州-綦江地震剖面;灯影组底拉平,剖面位置见图 8BB

      Fig.  14.  Typical 2D seismic profile of Dengying Formation in South Sichuan

      图  15  四川盆地不同地区震旦纪-早寒武世构造演化模式

      a.川北地区;b.川南地区.剖面位置见图 12

      Fig.  15.  The tectonic evolution model of Sinian-Early Cambrian in different regions of Sichuan Basin

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    • 收稿日期:  2018-10-25
    • 刊出日期:  2019-03-15

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