The earth's structure may change with time under natural or anthropogenic loading.Monitoring the subtle changes of the subsurface structure with repeatable seismic sources such as repeating earthquakes,ambient sei...The earth's structure may change with time under natural or anthropogenic loading.Monitoring the subtle changes of the subsurface structure with repeatable seismic sources such as repeating earthquakes,ambient seismic noise and artificial sources has become one of the hot topics in seismological research. These studies provide important clues in understanding the physical process of hazardous events such as earthquakes and volcanic eruptions. In this review we introduce the practices and advances in exploring and monitoring the subsurface structure with artificial seismic sources. This review is orgainzed as follows. Firstly,we describe the studies on the characteristics of different types of seismic source( especially the airgun source). Then the advances on data processing and mechanical understanding are depicted. At the end of this review,we reveal the prospects of future study of exploration and monitoring of the subsurface structure and its temporal variations using artificial sources.展开更多
This paper proposes the application of dynamic programming method to calculate the relative change of wave velocities and compares its similarities and differences with the cross-correlation delay estimation method ba...This paper proposes the application of dynamic programming method to calculate the relative change of wave velocities and compares its similarities and differences with the cross-correlation delay estimation method based on interference.The results show that:①the trend of wave velocities obtained by cross-correlation method and dynamic programming method are consistent.Besides,it is considered that the calculated result using cross-correlation delay method is reliable.②Compared with the cross-correlation delay method,the calculated result of the dynamic programming method has a magnifying effect and is more sensitive to small disturbances.③Under ideal conditions,the wave velocity change trend calculated by P-wave and S-wave phase should be consistent.In addition,the cross-correlation delay method is used to calculate the wave velocity change.Under appropriate conditions,the process of recovering from the suspected wave velocity before the M_L1.1 earthquake near the airgun source can be observed.展开更多
基金jointly sponsored by the Special Fundfor Earthquake Scientific Research(201508008)the National Natural Science Foundation of China(41474048,41474051,41561164018)Academician Chen Yong Workstation Project of Yunnan Province
文摘The earth's structure may change with time under natural or anthropogenic loading.Monitoring the subtle changes of the subsurface structure with repeatable seismic sources such as repeating earthquakes,ambient seismic noise and artificial sources has become one of the hot topics in seismological research. These studies provide important clues in understanding the physical process of hazardous events such as earthquakes and volcanic eruptions. In this review we introduce the practices and advances in exploring and monitoring the subsurface structure with artificial seismic sources. This review is orgainzed as follows. Firstly,we describe the studies on the characteristics of different types of seismic source( especially the airgun source). Then the advances on data processing and mechanical understanding are depicted. At the end of this review,we reveal the prospects of future study of exploration and monitoring of the subsurface structure and its temporal variations using artificial sources.
基金the Yunnan Youth Fund(2017K01)the Assistantship Project of the Yunnan Earthquake Agency
文摘This paper proposes the application of dynamic programming method to calculate the relative change of wave velocities and compares its similarities and differences with the cross-correlation delay estimation method based on interference.The results show that:①the trend of wave velocities obtained by cross-correlation method and dynamic programming method are consistent.Besides,it is considered that the calculated result using cross-correlation delay method is reliable.②Compared with the cross-correlation delay method,the calculated result of the dynamic programming method has a magnifying effect and is more sensitive to small disturbances.③Under ideal conditions,the wave velocity change trend calculated by P-wave and S-wave phase should be consistent.In addition,the cross-correlation delay method is used to calculate the wave velocity change.Under appropriate conditions,the process of recovering from the suspected wave velocity before the M_L1.1 earthquake near the airgun source can be observed.
