吉林大学学报(地球科学版) ›› 2016, Vol. 46 ›› Issue (3): 900-910.doi: 10.13278/j.cnki.jjuese.201603304

• 地球探测与信息技术 • 上一篇    下一篇


康健, 韦庆海, 周琳, 高研, 张永刚, 高峰   

  1. 黑龙江省地震局, 哈尔滨 150090
  • 收稿日期:2015-08-26 出版日期:2016-05-26 发布日期:2016-05-26
  • 作者简介:康健(1980),男,工程师,硕士,主要从事地震工程研究,E-mail:jakekj@163.com
  • 基金资助:


Deep Structure Based on Seismic Array Observations in Daqing Area

Kang Jian, Wei Qinghai, Zhou Lin, Gao Yan, Zhang Yonggang, Gao Feng   

  1. Earthquake Administration of Heilongjiang Province, Harbin 150090, China
  • Received:2015-08-26 Online:2016-05-26 Published:2016-05-26
  • Supported by:

    Supported by the Earthquake Industry Research Projects in China Earthquake Administration (1521044025)



关键词: 松辽盆地, 大庆地区, P波速度结构, S波速度结构, 层析成像


We combine the data from the mobile seismic array in Suifenhe-Manzhouli geoscience transect with those from the permanen tstations recorded from June, 2009 to May, 2011, the information are used for calculating the three-dimensional P-wave velocity structure of upper mantle in the study area according to body wave travel-time tomography, which is based on the limited frequency method.The proposed to mography method includes double-station phase velocity of Rayleigh wave and phase velocity of background noise, the three-dimensional S-wave velocity structure in the study area can be calculated by using the inversion. Finally, the two methods obtain the three-dimensional velocity distribution in Daqing area. The results show that the crust of Songliao basin is thin and the crusts of Da Hinggan Mountains and Xiao Hinggan Mountains around the Songliao basin are thick. The crust often has low velocity anomaly in the Songliao basin, the crust-mantle boundary and upper mantle show high velocity anomaly compared with the neighboring regions. The reason of local high-speed anomalies may be due to the rise of mantle material. Velocity anomalies usually show NS or NNE, which may be related to the impact of regional faults on the upper and middle crust.

Key words: Songliao basin, Daqing area, P-wave velocity structure, S-wave velocity structure, tomography


  • P631.4

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