
Discussion on the applicability of 90° phase conversion technique in seismic sedimentology
Author(s) -
Pengfei Zhao,
Xiaoliang Li,
Jingfeng Zong,
Fang Huang,
Jinhuang Wu,
Fei Yang,
Gaoming Yu,
Pengpeng Wei
Publication year - 2021
Publication title -
iop conference series. earth and environmental science
Language(s) - English
Resource type - Journals
eISSN - 1755-1307
pISSN - 1755-1315
DOI - 10.1088/1755-1315/692/4/042127
Subject(s) - sedimentology , geology , lithology , phase (matter) , synthetic seismogram , reflection (computer programming) , seismology , seismic to simulation , interpretation (philosophy) , seismic inversion , petrology , paleontology , geometry , computer science , chemistry , mathematics , organic chemistry , azimuth , programming language
Since 1998, domestic and foreign scholars have conducted more systematic research on the theory and application technology of seismic sedimentology, and 90° phase conversion has been proposed as one of the core technologies of seismic sedimentology. But in actual research and application, the technology has not achieved the expected results. The 90° phase conversion intends to give the meaning of the seismic reflection event representing the stratum interface to the lithologic strata by means of phase shift. Due to the complexity and change of the underground strata, there are usually multiple lithology frequent thin interbeds. Therefore, the event axis in the seismic profile is the combined effect of multiple sets of thin interbeds. The seismic data after 90° phase conversion cannot convert the original seismic data from interface seismic profile to lithologic stratigraphic profile, and lacks clear geological meaning. Its application ability in seismic structure interpretation and seismic lithology interpretation is very limited. Therefore, it is difficult to become an applied technology of seismic sedimentology. Therefore, it is not appropriate to use the 90° phase conversion technology as the core technology of seismic sedimentology. This technology neither improves the seismic data resolution capability nor accurately converts the seismic profile into a lithological profile.