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花海盆地深地震反射剖面的最佳采集参数实验和分析

王冠, 熊小松, 高锐, 陈宣华. 2019. 花海盆地深地震反射剖面的最佳采集参数实验和分析[J]. 中国地质, 46(5): 1146-1160. doi: 10.12029/gc20190515
引用本文: 王冠, 熊小松, 高锐, 陈宣华. 2019. 花海盆地深地震反射剖面的最佳采集参数实验和分析[J]. 中国地质, 46(5): 1146-1160. doi: 10.12029/gc20190515
WANG Guan, XIONG Xiaosong, GAO Rui, CHEN Xuanhua. 2019. Experiment and analysis of the best acquisition parameters for deep seismic reflection profiles in Huahai Basin[J]. Geology in China, 46(5): 1146-1160. doi: 10.12029/gc20190515
Citation: WANG Guan, XIONG Xiaosong, GAO Rui, CHEN Xuanhua. 2019. Experiment and analysis of the best acquisition parameters for deep seismic reflection profiles in Huahai Basin[J]. Geology in China, 46(5): 1146-1160. doi: 10.12029/gc20190515

花海盆地深地震反射剖面的最佳采集参数实验和分析

  • 基金项目:
    中国地质调查局项目(DD20179342,DD20160083),国家自然科学基金(41774114,41574093,41590860)和国家重点研发计划课题(2016YFC0600302)联合资助
详细信息
    作者简介: 王冠, 男, 1993年生, 硕士生, 研究方向:盆山结合带深部结构; E-mail:18500193419@163.com
    通讯作者: 熊小松, 男, 1983年生, 博士, 副研究员, 主要从事深部构造与大陆岩石圈演化研究; E-mail:benxung@126.com
  • 中图分类号: P631.4

Experiment and analysis of the best acquisition parameters for deep seismic reflection profiles in Huahai Basin

  • Fund Project: Supported by China Geological Survey Program (No. DD20179342, DD20160083), NSFC (No. 41774114, 41574093, 41590860) and National Key R&D Program of China (No. 2016YFC0600302)
More Information
    Author Bio: WANG Guan, male, born in 1993, master candidate, majors in research on the deep structure of basinmountain belt; E-mail:18500193419@163.com .
    Corresponding author: XIONG Xiaosong, male, born in 1983, associate professor, engages mainly in research on the deep structure and evolution of the continental lithosphere; E-mail: benxung@126.com
  • 深地震反射方法是探测地壳深部结构的先锋技术,能获取到莫霍面和上地幔的反射图像,成为揭示岩石圈结构、解决深部地质构造问题的有效手段。花海盆地位于河西走廊盆地群西部,处于不同大地构造单元的交汇部位,地层发育较全,但出露和发育程度差异较大,除白垩系为大面积连续分布外,其他各时代的地层均出露不全,常表现为被侵入岩分割破坏的残块状,为了确定深地震反射在花海盆地适合的采集参数,在采集前开展点试验,进行小、中、大炮炸药井炮激发参数对比优选,最终得到最优化的采集参数。在小炮实验中,36 kg药量取得的反射信息没有48 kg和60 kg的丰富,而且在MOHO反射的清晰度上48 kg和60 kg药量更为清晰,单井激发比组合井激发效果好;在中炮和大炮实验中,不同组合井对比差异不大,随着药量增大,激发能量增大,面波、折射波等干扰波能量也在增大,小炮干扰波能量最弱,反射信息最丰富的,中炮和大炮干扰波较发育,但通过后期去噪处理,也能得到中浅层反射信息。

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  • 图 1  花海盆地研究区以及周缘地区构造简图

    Figure 1. 

    图 2  花海盆地地质略图(据徐学义等,2009修改)

    Figure 2. 

    图 3  点试验接收排列高程图

    Figure 3. 

    图 4  小炮试验点接收排列地表高程图

    Figure 4. 

    图 5  小炮小折射记录及时距曲线

    Figure 5. 

    图 6  小炮单井自动增益

    Figure 6. 

    图 7  小炮单井低通滤波0~10 Hz

    Figure 7. 

    图 8  小炮单井带通滤波20~40 Hz

    Figure 8. 

    图 9  小炮组合井自动增益

    Figure 9. 

    图 10  小炮组合井低通滤波0~10 Hz

    Figure 10. 

    图 11  小炮组合井带通滤波20~40 Hz

    Figure 11. 

    图 12  中炮试验点接收排列地表高程图

    Figure 12. 

    图 13  中炮小折射记录及时距曲线

    Figure 13. 

    图 14  中炮组合井自动增益

    Figure 14. 

    图 15  中炮组合井低通滤波0~10 Hz

    Figure 15. 

    图 16  中炮组合井带通滤波20~40 Hz

    Figure 16. 

    图 17  大炮试验点接收排列地表高程图

    Figure 17. 

    图 18  大炮小折射记录及时距曲线

    Figure 18. 

    图 19  大炮组合井自动增益

    Figure 19. 

    图 20  大炮组合井低通滤波0~10 Hz

    Figure 20. 

    图 21  大炮组合井带通滤波10~20 Hz

    Figure 21. 

    表 1  实验对比内容

    Table 1.  Experimental comparison table

    下载: 导出CSV
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出版历程
收稿日期:  2019-03-18
修回日期:  2019-09-11
刊出日期:  2019-10-25

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