Journal of Tropical Oceanography ›› 2020, Vol. 39 ›› Issue (4): 80-90.doi: 10.11978/2019087CSTR: 32234.14.2019087

• Marine Geophysics • Previous Articles     Next Articles

Application of Kirchhoff downward-continued method to travel-time inversion of synthetic multi-channel seismic data

Maochuan ZHANG1,2,3(), Min XU1,3(), Xu ZHAO1,2,3, Jiazheng ZHANG1,3, Caicai ZHA1,2,3, M. V. P. Vithana1,2, Huizhe DI1,2,3, Xin ZENG1,3   

  1. 1. Key Laboratory of Ocean and Marginal Sea Geology, South China Sea Institute of Oceanology, Innovation Academy of South China Sea Ecology and Environmental Engineering, Chinese Academy of Sciences, Guangzhou 510301, China
    2. University of Chinese Academy of Sciences, Beijing 100049, China
    3. Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou), Guangzhou 511548, China
  • Received:2019-09-16 Revised:2020-01-17 Online:2020-07-20 Published:2020-07-27
  • Contact: Min XU E-mail:zhangmaochuan@scsio.ac.cn;mxu@scsio.ac.cn
  • Supported by:
    Foundation item: National Natural Science Foundation of China(41676044);Foundation item: National Natural Science Foundation of China(91858207);Foundation item: National Natural Science Foundation of China(41890813);The Strategic Priority Research Program of the Chinese Academy of Sciences(XDA13010105);Key Special Project for Introduced Talents Team of Southern Marine Science and Engineering Guangdong Laboratory(Guangzhou)(GML2019ZD0205)

Abstract:

Velocity model building and seismic imaging from marine multi-channel seismic (MCS) data are essential to obtain the structural information of oceanic crust. Existence of the seawater layer makes first-arrival refraction phases recorded by streamer only existed in far offset, while most of them in near offset are masked by the strong amplitude seafloor reflection phase, affecting travel-time picking and inversion. Based on the Kirchhoff integral approach to wave equation, we successfully implement the downward continuation (DC) method to the MCS data, and obtain first-arrival travel-time picks within a wider offset range. The method is applied to the synthetic MCS data simulated based on layer 2A/2B structure of newborn crust along a mid-ocean ridge, and first-arrival picking range and inversion result are compared before and after the DC. The DC method can expand offset range for first-arrival refraction picking and increase the ray coverage in the shallow depth, without changing the kinematics and dynamic characteristics of seismic wave field. The inversion results can more precisely distinguish the layer 2A/2B interface, and obtain higher resolution and more accurate velocity profile.

Key words: marine multi-channel seismic, Kirchhoff integration, downward continuation, travel-time inversion, oceanic crust layer 2A/2B

CLC Number: 

  • P738.4