It was concluded that the proper parameters for seismic mapping of complex structures in mountainous areas are that the datum should be horizontal plane, the static correction velocity the average velocity of the target formation, and the velocity of time-depth conversion be v_ (nl).
The interval velocity,time-depth conversion and sand content of the Zhongjiannan Basin in the South China Sea are calculated based on interpretation of velocity spectra.
The deep array induction well logging data can give a good approximation to the virgin resistivity when the thickness of the layer is over 1 m and the invasion radius is no more than 0.25 m.
8 weeks later, the colors of positive cells became deeper compared with that after 72 hours and the shape of the cells was irregularity, and the cells were significantly ageing.
(3) At [C%]<[C%]m (the lowest carbon content during decarburization) and [O%]<[O%]sat. (the saturated [O] content in liquid iron), the contents of carbon and oxygen in the melts are increased with blowing CO2 into the melts.
Time-depth recorders were attached to immature hawksbills (Eretmochelys imbricata Linnaeus, 1766) residing at the northwestern cliffs of Mona Island, Puerto Rico.
The pattern and characteristics of diving in 14 female northern rockhopper penguins, Eudyptes chrysocome moseleyi, were studied at Amsterdam Island (37°50'S; 77°31'E) during the guard stage, using electronic time-depth recorders.
In this study, time-depth recorders (TDRs) programmed to record temperature were deployed on female Antarctic fur seals (Arctocephalus gazella) at Bird Island, South Georgia (54°00'S; 38°02'W) during the breeding seasons 1994 to 1998.
Time-depth recorders were used to record dive duration, bottom duration, post-dive interval, ascent rate and descent rate in breeding adults during different seasons in 1995 and 1996.
In the case of constant formation velocity, F-K migration is a very simple and fast processing method, which first makes, in F-K domain, 2-D Fourier transform of wave equation to work out migration operator in F-K domain, then conducts, by replacing variable, a reverse 2-D Fourier transform of wave field at zero time to obtain migrated section. In principle, when formation velocity varies with depth, a stacked time section can still be transformed to pseudo depth section by using a given velocity curve, whi...
In this article, we investigate the propagation of direct and reflected seismic waves, and their anisotropy in a thin multilayered coherent 2-D solid model through model experimentation. By use of coordinate transformation, the multilayered anisotropic medium is changed into a homogeneous isotropic medium and a theoretical T-D equation of seismic reflection wave is derived. We present here the calculation method for the anisotropy factor and mapping method for the geological profile. Comparing the geologica...
In this paper, the F-K migration was examined from the view-point of transformation. By dint of the time-depth transformation, the F-K migration was made suitable for the state of variable velocity. Because of the data needed to process was always finite in length and discre-tized, it may produce the boundary effects at the end point and bring about the alias as well. Hence, the terms following related to the coordinate sys- terns should be taken into account carefully and seriously: the sampling intervals,...