六盘山盆地构造变形分析:来自地震剖面的约束

王建伟, 刘俊民, 张义平, 田连玉, 颜小宁, 丁丽荣. 2024. 六盘山盆地构造变形分析:来自地震剖面的约束. 地质通报, 43(11): 1937-1949. doi: 10.12097/gbc.2024.03.035
引用本文: 王建伟, 刘俊民, 张义平, 田连玉, 颜小宁, 丁丽荣. 2024. 六盘山盆地构造变形分析:来自地震剖面的约束. 地质通报, 43(11): 1937-1949. doi: 10.12097/gbc.2024.03.035
WANG Jianwei, LIU Junmin, ZHANG Yiping, TIAN Lianyu, YAN Xiaoning, DING Lirong. 2024. Tectonic deformation analysis of Liupanshan Basin: Constraints from seismic profiles. Geological Bulletin of China, 43(11): 1937-1949. doi: 10.12097/gbc.2024.03.035
Citation: WANG Jianwei, LIU Junmin, ZHANG Yiping, TIAN Lianyu, YAN Xiaoning, DING Lirong. 2024. Tectonic deformation analysis of Liupanshan Basin: Constraints from seismic profiles. Geological Bulletin of China, 43(11): 1937-1949. doi: 10.12097/gbc.2024.03.035

六盘山盆地构造变形分析:来自地震剖面的约束

  • 基金项目: 中国地质调查局项目《深部地质调查》(编号:DD20230008)、《西北重要构造廊带深部地质调查》(编号:DD20230229)、《鄂尔多斯盆地及周缘地质构造调查》(编号:DD20242780)、中石化科研攻关项目《柴达木及河西走廊地区油气资源潜力及选区评价》(编号:P22065)、中国地质科学院基本科研业务费项目《印支期华南北汇聚及前陆盆地形成的构造物理模拟》(编号:JKYQN202301)
详细信息
    作者简介: 王建伟(1975− ),男,博士,研究员,从事压扭盆地构造解释和油气勘探工作。E−mail:wangjianwei773.slyt@sinopec.com
    通讯作者: 张义平(1988− ),男,博士,高级工程师,从事构造地质和盆山耦合分析等研究工作。E−mail:BJZhYP@126.com
  • 中图分类号: P542;P631.4

Tectonic deformation analysis of Liupanshan Basin: Constraints from seismic profiles

More Information
  • 六盘山盆地先后经历早古生代克拉通碳酸盐岩台地、古生代海陆交互、中生代内陆湖盆等过程,发育石炭系、三叠系—侏罗系和白垩系3套烃源岩,是当下可拓展的油气有利区之一。但是,该盆地所处大地构造位置特殊,受青藏高原、阿拉善、鄂尔多斯等块体相互作用,经历多期构造运动,发育大量褶皱与断裂等构造,地壳结构及盆地属性经历强烈改造,在一定程度上制约了六盘山盆地油气资源评价和有利区带优选。基于此,选择六盘山盆地3条关键地震剖面,结合野外构造变形特征和钻井信息,讨论了六盘山盆地中生代以来多期构造事件下的盆山演化过程,主要包括中生代早期(三叠纪/侏罗纪)局部伸展断陷,早白垩世早期挤压与晚期伸展,新生代以来受青藏高原增生扩展,六盘山地区强烈挤压,造就了现今六盘山褶皱逆冲带。

  • 加载中
  • 图 1  研究区构造体系图

    Figure 1. 

    图 2  六盘山盆地及邻区地质与断裂分布

    Figure 2. 

    图 3  六盘山盆地3条关键地震剖面(剖面位置见图2。圆圈内数字为不同地震同相轴反射区,其中区域1为浅表第四系,区域2为沉积盖层,区域3为盆地基底;黄色箭头为沉积地层与盆地基底之间的边界;红色箭头为地震同相轴不连续处,反映断层等信息;蓝色箭头为盆地基底内反射)

    Figure 3. 

    图 4  六盘山盆地北东—南西走向地震剖面(1-1’)构造解译(剖面位置见图2

    Figure 4. 

    图 5  六盘山盆地北东—南西走向2-2’地震剖面构造解译(剖面位置见图2

    Figure 5. 

    图 6  寺口子下白垩统乃家河组(K1n)逆冲到渐新统清水营组(E3q)之上(露头位置见图5

    Figure 6. 

    图 7  六盘山盆地北西—南东走向3-3’地震剖面构造解译(剖面位置见图2

    Figure 7. 

    图 8  王家川上侏罗统挤压作用形成的生长地层

    Figure 8. 

    表 1  六盘山地区地层系统

    Table 1.  Stratigraphic stratum of the Liupanshan region

    下载: 导出CSV

    表 2  地震剖面数据采集与观测系统

    Table 2.  Seismic profile data acquisition and observation system

    项目 参数
    观测系统 2L1S
    排列方式 5990-10-20-10-5990
    CMP线元 10 m
    覆盖次数 100次×2=200次
    接收道数 600道×2=1200道
    道距 20 m
    炮点距 60 m
    接收线距 80 m
    最大炮检距 5990 m
    下载: 导出CSV
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出版历程
收稿日期:  2024-03-21
修回日期:  2024-04-26
刊出日期:  2024-11-15

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