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Way to calculate travel times FOR finite-frequency seismic migration software monochromatic wave fields

机译:有限频率地震偏移软件单色波场的传播时间计算方法

摘要

1. method u0434u043bu00a0 u043eu043fu0440u0435u0434u0435u043bu0435u043du0438u00a0 time of seismic waves on the surface of the item to the at least one point calculations within a multitude of points available u0438u00a0 in geological environment, including u0441u0435u0431u00a0:;(a) an area assignment models, including the many points u0441u0435u0431u00a0 u0440u0430u0437u043cu0435u0449u0435u043du0438u00a0 in geological environment.;(b) the calculation of u043cu043eu043du043eu0445u0440u043eu043cu0430u0442u0438u0447u0435u0441u043au043eu0433u043e wave speed model u0434u043bu00a0 u043fu043eu043bu00a0 using at least one point calculations.;(c) the definition of open phase of seismic waves in at least one of the point of computing, the nearest to the at least one point calculations in the specified u0440u0430u0437u043cu0435u0449u0435u043du0438u00a0 by multiple points; and;(d) determination of the time of seismic waves to the at least one point calculations in the defined open phase and the u0432u044bu0447u0438u0441u043bu0435u043du043du043eu043cu0443 u043cu043eu043du043eu0445u0440u043eu043cu0430u0442u0438u0447u0435u0441u043au043eu043cu0443 u0432u043eu043bu043du043eu0432u043eu043cu0443 field u0434u043bu00a0 at least one point calculations.;2. method for 1, in which the point on the surface of u043fu0440u0435u0434u0441u0442u0430u0432u043bu00a0u0435u0442 one of: (i) and (ii) u043cu0435u0441u0442u043eu043fu043eu043bu043eu0436u0435u043du0438u00a0 u043cu0435u0441u0442u043eu043fu043eu043bu043eu0436u0435u043du0438u00a0 source receiver.;3. method for p.1, in which the calculation u043cu043eu043du043eu0445u0440u043eu043cu0430u0442u0438u0447u0435u0441u043au043eu0433u043e wave u043fu043eu043bu00a0 u0434u043bu00a0 at least one point calculations further includes u0441u0435u0431u00a0 definition u043cu043eu043du043eu0445u0440u043eu043cu0430u0442u0438u0447u0435u0441u043au043eu0433 on the u0440u0435u0448u0435u043du0438u00a0 u0434u043bu00a0 of at least one of: (i) the wave u0443u0440u0430u0432u043du0435u043du0438u00a0 elastic waves u0434u043bu00a0 runs in one direction, (ii) the wave u0443u0440u0430u0432u043du0435u043du0438u00a0 elastic waves u0434u043bu00a0 full mileage and, the(iii) the wave u0443u0440u0430u0432u043du0435u043du0438u00a0 acoustic waves u0434u043bu00a0 runs in one direction, and (iv) the wave u0443u0440u0430u0432u043du0435u043du0438u00a0 acoustic waves u0434u043bu00a0 total mileage.;4. method for calculation of wave 3, which u043cu043eu043du043eu0445u0440u043eu043cu0430u0442u0438u0447u0435u0441u043au043eu0433u043e u043fu043eu043bu00a0 further includes u0441u0435u0431u00a0 process u0440u0435u0448u0435u043du0438u00a0 u0434u043bu00a0 u043du0430u0445u043eu0436u0434u0435u043du0438u00a0 solutions for wave u0443u0440u0430u0432u043du0435u043du0438u00a0 at least one of: (i) the method of finite element, (ii) the method of finite u0440u0430u0437u043du043eu0441u0442u0435u0439, (iii) and (iv) u00a0u0432u043du043eu0433u043e method u043du0435u00a0u0432u043du043eu0433u043e method.;5. method for calculation of wave 3, which u043cu043eu043du043eu0445u0440u043eu043cu0430u0442u0438u0447u0435u0441u043au043eu0433u043e u043fu043eu043bu00a0 further includes the use of at least one function u0441u0435u0431u00a0 greene.;6. method for article 3, which additionally includes u0441u0435u0431u00a0 receive the amplitude coefficients of the migration on the basis of u0432u044bu0447u0438u0441u043bu0435u043du043du043eu0433u043e u043cu043eu043du043eu0445u0440u043eu043cu0430u0442u0438u0447u0435u0441u043au043eu0433u043e u0432u043eu043bu043du043eu0432u043e laplacian the u043fu043eu043bu00a0.;7. method for 1, in which at least one point to many points u0441u0435u0431u00a0 computation includes computing.;8. method for 1, in which at least one u0441u043eu0441u0435u0434u043du00a0u00a0 point computing includes u0441u0435u0431u00a0 many neighbouring points calculation.;9. method for 1, which further includes u0441u0435u0431u00a0 definition on the basis of at least one u0432u044bu0447u0438u0441u043bu0435u043du043du043eu0433u043e time of at least one of: (i) cards the mileage and (ii) the table of distance.;10. method for 1, in which at least one u0441u043eu0441u0435u0434u043du00a0u00a0 point computing includes u0441u0435u0431u00a0 many neighbouring points calculations, and the method further includes u0441u0435u0431u00a0 the definition of the phases of the neighbouring points calculations by u043eu0431u0440u0430u0437u043eu0432u0430u043du0438u00a0 weighted sum of the phases of the neighbouring points calculation.;11. method for 1, in which the definition of the open phase of at least one point computing includes u0441u0435u0431u00a0 limitation of open phase, at least one is ci calculations within a certain phase u0434u043bu00a0 at least one neighbouring point calculations.;12. method for 1, in which the definition of time further includes u0441u0435u0431u00a0 calculation u043cu043eu043du043eu0445u0440u043eu043cu0430u0442u0438u0447u0435u0441u043au043eu0433u043e wave u043fu043eu043bu00a0 on multidimensional surfaces.;13. method for 1, in which the definition of time further includes u0441u0435u0431u00a0 calculation u043cu043eu043du043eu0445u0440u043eu043cu0430u0442u0438u0447u0435u0441u043au043eu0433u043e wave u043fu043eu043bu00a0 on multidimensional surfaces that u0440u0430u00a0 u043fu0440u0435u0434u0441u0442u0430u0432u043bu00a0u0435u0442 a u0434u0432u0430u0434u0446u0430u0442u0438u0433u0440u0430u043du043du0438u043a.;14. method for p.1, in which the definition of the time of seismic waves to the at least one point calculations further includes u0441u0435u0431u00a0, at least one of: (i) anal isa local gradient time, (ii) analysis of the local gradient u043du0435u0440u0430u0437u0432u0435u0440u043du0443u0442u043eu0439 phase, (iii) u043eu043fu0440u0435u0434u0435u043bu0435u043du0438u00a0 the highest amplitude of at least one neighbouring the calculations(iv) the definition of the least open phase of at least one of the point of computing, (v) a flat wave u0434u043bu00a0 of at least one other point you u0447u0438u0441u043bu0435u043du0438u0439, (vi) the weighted plane wave u0434u043bu00a0 at least one neighbouring point calculations, and (vii) the calculation of weighted wave impulse u0433u044eu0439u0433u0435u043du0441u0430 on u0441u043du043eu0432u0430u043du0438u0438 at least one neighbouring point calculations.;15. method u0434u043bu00a0 u043eu043fu0440u0435u0434u0435u043bu0435u043du0438u00a0 maps of seismic waves from u0434u043bu00a0 running item on a surface and at least one point calculations within the many points u0440u0430u0437u043cu0435u0449u0435u043du0438u00a0 in geological environment, including u0441u0435u0431u00a0:;(a) an area assignment models, including the many points u0441u0435u0431u00a0 u0440u0430u0437u043cu0435u0449u0435u043du0438u00a0 in geological environment.;(b) the calculation of u043cu043eu043du043eu0445u0440u043eu043cu0430u0442u0438u0447u0435u0441u043au043eu0433u043e wave speed model u0434u043bu00a0 u043fu043eu043bu00a0 using at least one point calculations.;(c) the definition of open phase of seismic waves in at least one of the point of computing, the nearest to the at least one point calculations in the specified u0440u0430u0437u043cu0435u0449u0435u043du0438u00a0 by multiple points;;(d) determination of the time of seismic waves to the at least one point calculations in the defined open phase and the u0432u044bu0447u0438u0441u043bu0435u043du043du043eu043cu0443 u043cu043eu043du043eu0445u0440u043eu043cu0430u0442u0438u0447u0435u0441u043au043eu043cu0443 u0432u043eu043bu043du043eu0432u043eu043cu0443 field u0434u043bu00a0 at least one point calculations.;(e) the values of the distance in the form of a map.;16. method for p.15, which the point on the surface of u043fu0440u0435u0434u0441u0442u0430u0432u043bu00a0u0435u0442 one of: (i) and (ii) u043cu0435u0441u0442u043eu043fu043eu043bu043eu0436u0435u043du0438u00a0 u043cu0435u0441u0442u043eu043fu043eu043bu043eu0436u0435u043du0438u00a0 source receiver.;17. method for p.15, wherein at least one point to many points u0441u0435u0431u00a0 computation includes computing.;18. method for p.15, wherein at least one u0441u043eu0441u0435u0434u043du00a0u00a0 point computing includes u0441u0435u0431u00a0 many neighbouring points calculation.;19. method for p.15, wherein at least one u0441u043eu0441u0435u0434u043du00a0u00a0 point computing includes u0441u0435u0431u00a0 many neighbouring points calculations, and the method further includes u0441u0435u0431u00a0 the definition of the phases of the neighbouring points calculations by u0444u043eu0440u043cu0438u0440u043eu0432u0430u043du0438u00a0 weighted sum of the phases of the neighbouring points calculation.;20. method for determination of open phase, p.15, in which at least one point computing includes u0441u0435u0431u00a0 limitation of open phase, at least one u0447u043au0438 calculations within a certain phase u0434u043bu00a0 at least one neighbouring point calculations.;21. method for u043eu043fu0440u0435u0434u0435u043bu00a0u0435u043cu043eu0435 p.15, which u043cu043eu043du043eu0445u0440u043eu043cu0430u0442u0438u0447u0435u0441u043au043eu0435 wave field u0432u044bu0447u0438u0441u043bu00a0u044eu0442, u0438u0441u043fu043eu043bu044cu0437u0443u00a0 at least one function green.;22. method for p.15, which additionally includes u0441u0435u0431u00a0 receive the amplitude coefficients of the migration on the basis of u0432u044bu0447u0438u0441u043bu0435u043du043du043eu0433u043e u043cu043eu043du043eu0445u0440u043eu043cu0430u0442u0438u0447u0435u0441u043au043eu0433u043e u0432u043eu043bu043du043eu0432u043e laplacian the u043fu043eu043bu00a0.;23. method for determination of u043cu043eu043du043eu0445u0440u043eu043cu0430u0442u0438u0447u0435u0441u043au043eu0433u043e p.15, in which the wave u043fu043eu043bu00a0 further includes u0441u0435u0431u00a0 calculation of wave u043fu043eu043bu00a0 on multidimensional surfaces.;24. method for determination of u043cu043eu043du043eu0445u0440u043eu043cu0430u0442u0438u0447u0435u0441u043au043eu0433u043e p.15, in which the wave u043fu043eu043bu00a0 further includes u0441u0435u0431u00a0 calculation of wave u043fu043eu043bu00a0 on multidimensional surfaces that u0440u0430u00a0 u043fu0440u0435u0434u0441u0442u0430u0432u043bu00a0u0435u0442 a u0434u0432u0430u0434u0446u0430u0442u0438u0433u0440u0430u043du043du0438u043a.;25. method for p.15, in which the definition of u043cu043eu043du043eu0445u0440u043eu043cu0430u0442u0438u0447u0435u0441u043au043eu0433u043e wave u043fu043eu043bu00a0 further includes u0441u0435u0431u00a0 u0440u0435u0448u0435u043du0438u00a0 u0434u043bu00a0 calculation of at least one of: (i) the wave u0443u0440u0430u0432u043du0435u043du0438u00a0 elastic waves u0434u043bu00a0 runs in one direction, (ii) the wave u0443u0440u0430u0432u043du0435u043du0438u00a0 elastic waves u0434u043bu00a0 total mileage.(iii) the wave u0443u0440u0430u0432u043du0435u043du0438u00a0 acoustic waves u0434u043bu00a0 runs in one direction, and (iv) the wave u0443u0440u0430u0432u043du0435u043du0438u00a0 acoustic waves u0434u043bu00a0 total mileage.;26. method for determination of u043cu043eu043du043eu0445u0440u043eu043cu0430u0442u0438u0447u0435u0441u043au043eu0433u043e p.15, in which the wave u043fu043eu043bu00a0 further includes u0441u0435u0431u00a0 process u0440u0435u0448u0435u043du0438u00a0 u0434u043bu00a0 u043du0430u0445u043eu0436u0434u0435u043du0438u00a0 solutions u0443u0440u0430u0432u043du0435u043du0438u00a0 wave at least one of: (i) the method of finite u0440u0430u0437u043du043eu0441u0442u0435u0439, (ii) the method of finite element method u00a0u0432u043du043eu0433u043e, (iii), (iv) and (v) u043du0435u00a0u0432u043du043eu0433u043e method u043fu0440u0435u043eu0431u0440u0430u0437u043eu0432u0430u043du0438u00a0 fourier method.;27. method for p.15, in which the definition of the time of seismic waves to the at least one point calculations further includes u0441u0435u0431u00a0, at least one of: (i) anal isa local gradient time, (ii) analysis of the local gradient u043du0435u0440u0430u0437u0432u0435u0440u043du0443u0442u043eu0439 phase, (iii) u043eu043fu0440u0435u0434u0435u043bu0435u043du0438u00a0 the highest amplitude of at least one neighbouring the calculations(iv) the definition of the least open phase of at least one of the point of computing, (v) a flat wave u0434u043bu00a0 of at least one other point you u0447u0438u0441u043bu0435u043du0438u0439, (vi) the weighted plane wave u0434u043bu00a0 at least one neighbouring point calculations, and (vii) the calculation of weighted wave impulse u0433u044eu0439u0433u0435u043du0441u0430 on u0441u043du043eu0432u0430u043du0438u0438 at least one neighbouring point calculations.;28. method u0434u043bu00a0 u043eu043fu0440u0435u0434u0435u043bu0435u043du0438u00a0 time of seismic waves on the surface of the item to the at least one point calculations within a multitude of points available u0438u00a0 in geological environment, including u0441u0435u0431u00a0:;(a) an area assignment models, including the many points u0441u0435u0431u00a0 u0440u0430u0437u043cu0435u0449u0435u043du0438u00a0 in geological environment.;(b) the calculation of the wave u043fu043eu043bu00a0 u0434u043bu00a0 of at least one selected frequencies using the fast model u0434u043bu00a0 at least one point calculations.;(c) the definition of open phase of seismic waves in at least one of the point of computing, the nearest to the at least one point calculations in the specified u0440u0430u0437u043cu0435u0449u0435u043du0438u00a0 by multiple points; and;(d) determination of the time of seismic waves to the at least one point calculations in the defined open phase and the u0432u044bu0447u0438u0441u043bu0435u043du043du043eu043cu0443 u0432u043eu043bu043du043eu0432u043eu043cu0443 field u0434u043bu00a0 at least one point calculations.;29. method for p.28, which the point on the surface of u043fu0440u0435u0434u0441u0442u0430u0432u043bu00a0u0435u0442 one of: (i) u043cu0435u0441u0442u043eu043fu043eu043bu043eu0436u0435u043du0438u00a0 source, and (ii) u043cu0435u0441u0442u043eu043fu043eu043bu043eu0436u0435u043du0438u00a0 receiver.;30. method for p.28, in which the calculation of the wave u043fu043eu043bu00a0 u0434u043bu00a0 at least one point calculations further includes a u0441u0435u0431u00a0 u0440u0435u0448u0435u043du0438u00a0 u043fu043eu043bu00a0 to wave at me re the one selected frequency u0434u043bu00a0 of at least one of: (i) the wave u0443u0440u0430u0432u043du0435u043du0438u00a0 elastic waves u0434u043bu00a0 runs in one direction, (ii) the wave u0443u0440u0430u0432u043du0435u043du0438u00a0 elastic waves d u043bu00a0 total mileage.(iii) the wave u0443u0440u0430u0432u043du0435u043du0438u00a0 acoustic waves u0434u043bu00a0 runs in one direction, and (iv) the wave u0443u0440u0430u0432u043du0435u043du0438u00a0 acoustic waves u0434u043bu00a0 total mileage.;31. method for calculating u043cu043eu043du043eu0445u0440u043eu043cu0430u0442u0438u0447u0435u0441u043au043eu0433u043e p.30 in which wave u043fu043eu043bu00a0 further includes u0441u0435u0431u00a0 process u0440u0435u0448u0435u043du0438u00a0 u0434u043bu00a0 u043du0430u0445u043eu0436u0434u0435u043du0438u00a0 solutions u0443u0440u0430u0432u043du0435u043du0438u00a0 p wave on at least one of: (i) the method of finite element, (ii) the method of finite u0440u0430u0437u043du043eu0441u0442u0435u0439, (iii) and (iv) u00a0u0432u043du043eu0433u043e method u043du0435u00a0u0432u043du043eu0433u043e method.;32. method for calculating the wave u043fu043eu043bu00a0 p.30 in which further includes the use of at least one function u0441u0435u0431u00a0 green u0434u043bu00a0 at least one pass u043du043du043eu0439 frequencies.;33. method for p.30, which additionally includes u0441u0435u0431u00a0 receive the amplitude coefficients of migration based on wave u043fu043eu043bu00a0 u0432u044bu0447u0438u0441u043bu0435u043du043du043eu0433u043e laplacian.;34. method for p.28, wherein at least one point to many points u0441u0435u0431u00a0 computation includes computing.;35. method for p.28, wherein at least one u0441u043eu0441u0435u0434u043du00a0u00a0 point computing includes u0441u0435u0431u00a0 many neighbouring points calculation.;36. method for p.28, which additionally includes u0441u0435u0431u00a0 definition on the basis of at least one u0432u044bu0447u0438u0441u043bu0435u043du043du043eu0433u043e time of at least one of: (i) cards the mileage and (ii) the table of distance.;37. method for p.28, wherein at least one u0441u043eu0441u0435u0434u043du00a0u00a0 point computing includes u0441u0435u0431u00a0 many neighbouring points calculations, and the method further includes u0441u0435u0431u00a0 the definition of the phases of the neighbouring points calculations by u043eu0431u0440u0430u0437u043eu0432u0430u043du0438u00a0 weighted sum of the phases of the neighbouring points calculation.;38. method for determination of open phase, p.28, in which at least one point computing includes u0441u0435u0431u00a0 limitation of open phase, at least one u0447u043au0438 calculations within a certain phase u0434u043bu00a0 at least one neighbouring point calculations.;39. method for 1, in which the definition of time further includes u0441u0435u0431u00a0 wave u043fu043eu043bu00a0 u0434u043bu00a0 calculation of at least one of the selected frequency in u043cu043du043eu0433u043eu0433 ranna surface.;40. method for 1, in which the definition of time further includes u0441u0435u0431u00a0 wave u043fu043eu043bu00a0 u0434u043bu00a0 calculation of at least one of the selected frequency in u043cu043du043eu0433u043eu0433 ranna surface u043au043eu0442u043eu0440u0430u00a0 u043fu0440u0435u0434u0441u0442u0430u0432u043bu00a0u0435u0442 a u0434u0432u0430u0434u0446u0430u0442u0438u0433u0440u0430u043du043du0438u043a.;41. method for p.15, in which the definition of the time of seismic waves to the at least one point calculations further includes u0441u0435u0431u00a0, at least one of: (i) anal isa local gradient time, (ii) analysis of the local gradient u043du0435u0440u0430u0437u0432u0435u0440u043du0443u0442u043eu0439 phase, (iii) u043eu043fu0440u0435u0434u0435u043bu0435u043du0438u00a0 the highest amplitude of at least one neighbouring the calculations(iv) the definition of the least open phase of at least one of the point of computing, (v) a flat wave u0434u043bu00a0 of at least one other point you u0447u0438u0441u043bu0435u043du0438u0439, (vi) the weighted plane wave u0434u043bu00a0 at least one neighbouring point calculations, and (vii) the calculation of weighted wave impulse u0433u044eu0439u0433u0435u043du0441u0430 on u0441u043du043eu0432u0430u043du0438u0438 at least one neighbouring point calculations.
机译:1.方法地震波在物体表面至少一点内的计算时间为 u0434 u043b u00a0 u043e u043f u0440 u0435 u0434 u0435 u043b u0435 u043d u0438 u00a0地质环境中可用的多个点 u0438 u00a0,包括 u0441 u0435 u0431 u00a0 :;(a)区域分配模型,包括许多点 u0441 u0435 u0431 u00a0 u0440 u0430 u0437 u043c u0435 u0449 u0435 u043d u0438 u00a0;(b) u043c u043e u043d u043e u0445 u0440 u043e u043c u0430 u0442 u0438 u0447 u0435的计算 u0441 u043a u043e u0433 u043e波速模型 u0434 u043b u00a0 u043f u043e u043b u00a0使用至少一个点计算;(c)至少一个地震波的开放相位定义计算点数,最接近指定的 u0440 u0430 u0437 u043c u0435 u0449 u0435 u043d u0438 u00a0中至少一个点计算; (d)确定在定义的开放相位和 u0432 u044b u0447 u0438 u0441 u043b u0435 u043d u043d u043d u043e u043c u0443中至少计算一次地震波的时间 u043c u043e u043d u043e u0445 u0440 u043e u043c u0430 u0442 u0438 u0447 u0435 u0441 u043a u043e u043c u0443 u0432 u043e u043b u043d u043e u0432 u043c u0443字段 u0434 u043b u00a0至少计算一个点; 2。 1的方​​法,其中 u043f u0440 u0435 u0434 u0441 u0442 u0430 u0432 u043b u00a0 u0435 u0442表面上的点:(i)和(ii) u043c u0435 u0441 u0442 u043e u043f u043e u043b u043e u0436 u0435 u043d u043d u0438 u00a0 u043c u0435 u0441 u0442 u043e u043f u043e u043e u043b u043e u0436 u0435 u043d u00a0源接收器; 3。第1页的方法,其中计算 u043c u043e u043d u043e u0445 u0440 u043e u043c u04c u0430 u0442 u0438 u0447 u0435 u0441 u043a u043e u043e u0433 u043e wave u043f u043e u043b u00a0 u0434 u043b u00a0至少一个点计算还包括 u0441 u0435 u0431 u00a0定义 u043c u043e u043d u043e u0445 u0440 u04340 u043e u043c u0430 u0442 u0438 u0440 u0435 u0448 u0435 u043d u0438 u00a0 u0434 u043b u00a0上的u0447 u0435 u0441 u043a u043e u0433至少其中之一:(i)波浪 u0443 u0440 u0430 u0432 u043d u0435 u043d u0438 u00a0弹性波 u0434 u043b u00a0沿一个方向传播,(ii)波浪 u0443 u0440 u0430 u0432 u043d u0435 u043d u043d u0438 u00a0弹性波 u0434 u043b u00a0全程行驶,并且(iii)声波 u0443 u0440 u0430 u0432 u043d u0435 u043d u0438 u00a0声波 u0434 u043b u00a0沿一个方向传播,并且(iv )声波 u0443 u0440 u0430 u0432 u043d u0435 u043d u0438 u00a0声波 u0434 u043b u00a0总英里数; 4。波浪3的计算方法,其中 u043c u043e u043d u043e u0445 u0440 u043e u043c u04c u0430 u0442 u0438 u0447 u0435 u0441 u043a u043e u0433 u0433 u043e u043f u043e u043b u00a0还包括 u0441 u0435 u0431 u00a0进程 u0440 u0435 u0448 u0435 u043d u0438 u00a0 u0434 u043b u00a0 u043d u0430 u0445 u04345 u043e u0436 u0434 u0435 u0435波浪 u0443 u0440 u0430 u0432 u043d u0435 u043d u0438 u00a0的u0438 u00a0解决方案至少以下之一:(i)有限元方法,(ii)有限 u0440 u0430 u0437 u043d u043e u0441 u0442 u0435 u0439,(iii)和(iv) u00a0 u0432 u043d u043e u0433 u043e方法 u043d u0435 u00a0 u0432 u043d u043e u0433 u043e方法; 5。波浪3的计算方法,其中 u043c u043e u043d u043e u0445 u0440 u043e u043c u04c u0430 u0442 u0438 u0447 u0435 u0441 u043a u043e u0433 u0433 u043e u043f u043e u043b u00a0还包括使用至少一个功能。 u0441 u0435 u0431 u00a0 greene .; 6。第3条的方法,其中还包括 u0441 u0435 u0431 u00a0,根据 u0432 u044b u0447 u0438 u0441 u043b u0435 u043d u043d u043e u0433 接收迁移的幅度系数u043e u043c u043e u043d u043e u0445 u0440 u043e u043c u0430 u0442 u0438 u0447 u0435 u0441 u043a u043e u0433 u043e u043e u0432 u043e u043b u043d u043e u043e la043f u043e u043b u00a0。; 7。 1的方​​法,其中至少一个点到许多点的计算包括计算。8。 1的方​​法,其中至少一个 u0441 u043e u0441 u0435 u0434 u043d u00a0 u00a0点计算包括 u0441 u0435 u0431 u00a0许多相邻点计算。 1的方​​法,其中还包括基于至少一个 u0432 u044b u0447 u0438 u0441 u043b u0435 u043d u043d u043d u043e u0433 u043e的时间定义 u0441 u0435 u0431 u00a0至少以下之一:(i)记录里程和(ii)距离表;; 10。 1的方​​法,其中至少一个 u0441 u043e u0441 u0435 u0434 u043d u00a0 u00a0点计算包括 u0441 u0435 u0431 u00a0许多相邻点计算,并且该方法还包括 u0441 u0435 u0431 u00a0通过 u043e u0431 u0440 u0430 u0437 u043e u0432 u0430 u043d u0438 u00a0的加权总和来定义相邻点的相位相邻点计算的阶段; 11。 1的方​​法,其中至少一个点计算的开放相的定义包括 u0441 u0435 u0431 u00a0的开放相限,至少一个是某一相内的ci计算 u0434 u043b u00a0至少一相邻点计算; 12。 1的方​​法,其中时间的定义还包括 u0441 u0435 u0431 u00a0计算 u043c u043e u043d u043e u0445 u0440 u043e u043c u04c u0430 u0442 u0438 u0447 u0435 u0441 在多维表面上的波 u043f u043e u043b u00a0; 13。 1的方​​法,其中时间的定义还包括 u0441 u0435 u0431 u00a0计算 u043c u043e u043d u043e u0445 u0440 u043e u043c u04c u0430 u0442 u0438 u0447 u0435 u0441 u043a u043e u0433 u043e在 u0440 u0430 u00a0 u043f u0440 u0435 u0434 u0441 u0441 u0442 u0430 u0432 u043b u00a0 u0435的多维表面上的波浪 u043f u043e u043b u00b0 u0434 u0432 u0430 u0434 u0446 u0430 u0442 u0438 u0433 u0440 u0430 u043d u043d u0438 u043a。; 14。 p.1的方法,其中地震波到至少一个点计算的时间的定义还包括 u0441 u0435 u0431 u00a0,其中至少一个是:(i)肛门isa局部梯度时间,(ii )分析局部梯度 u043d u0435 u0440 u0430 u0437 u0432 u0435 u0440 u043d u0443 u0442 u043e u0439相位,(iii) u043e u043f u0440 u04340 u0435 u0434 u0435 u043b u0435 u043d u0438 u00a0与计算相邻的至少一个最大振幅(iv)至少一个计算点的最小开相的定义,(v)平面波至少一个其他点的u00a0您是 u0447 u0438 u0441 u043b u0435 u043d u0438 u0439,(vi)加权平面波 u0434 u043b u00a0至少有一个相邻点计算,并且(vii)在至少一个相邻点计算上,在 u0441 u043d u043e u0432 u0430 u043d u0438 u0438上计算加权波脉冲 u0433 u044e u0439 u0433 u0435 u043d u0441 u0430; 15。方法 u0434 u043b u00a0 u043e u043f u0440 u0435 u0434 u0435 u043b u0435 u043d u0438 u00a0来自地面上至少有一个点的运行项 u0434 u043b u00a0的地震波图地质环境中包括 u0441 u0435 u0431 u00a0在内的多个点 u0440 u0430 u0437 u043c u0435 u0449 u0435 u043d u00a0内的计算:(a)区域分配模型,包括在地质环境中很多点 u0441 u0435 u0431 u00a0 u0440 u0430 u0437 u043c u0435 u0449 u0435 u043d u0438 u00a0;(b) u043c u043e u043d u043e u0445 u0440 u043e u043c u0430 u0442 u0438 u0447 u0435 u0441 u043a u043e u0433 u043e波速模型 u0434 u043b u00a0 u043f u043e u043b u00a0使用至少一个点计算。;(c)在指定的 u0440 u0430 u0437 u043c u0435 u0449 u0435 中至少一个计算点(最接近至少一个计算点)定义地震波的开放相位。 u043d u0438 u00a0多点;;(d)确定在定义的开放相位和 u0432 u044b u0447 u0438 u0441 u043b u0435 u043d u043d u043e u043c u0443 u043c u043e u043d u043e u0445 u0440 u043e u043c u0430 u0442 u0438 u0447 u0435 u0441 u043a u043e u043e u043c u0443 u0432 u043e u043b u043d u043d u043e u0432 u043e u043c u043c至少一个点计算;(e)以地图形式的距离值; 16。第15页的方法,其中 u043f u0440 u0435 u0434 u0441 u0442 u0430 u0432 u043b u00a0 u0435 u0442的表面上的点:(i)和(ii) u043c u0435 u0441 u0442 u043e u043f u043e u043b u043e u0436 u0435 u043d u043d u0438 u00a0 u043c u0435 u0441 u0442 u043e u043f u043e u043e u043b u043e u0436 u0435 u0438 u00a0源接收器;; 17。 p.15的方法,其中至少一个点到许多点的计算包括计算。18。 p.15的方法,其中至少一个 u0441 u043e u0441 u0435 u0434 u043d u00a0 u00a0点计算包括 u0441 u0435 u0431 u00a0许多相邻点计算。 p.15的方法,其中至少一个 u0441 u043e u0441 u0435 u0434 u043d u00a0 u00a0点计算包括 u0441 u0435 u0431 u00a0许多相邻点计算,并且该方法还包括 u0441 u0435 u0431 u00a0通过 u0444 u043e u0440 u043c u0438 u0440 u043e u0432 u0430 u043d u0438 u00a0定义相邻点计算相位的相位。; 20。确定缺相的方法,第15页,其中至少一个点计算包括 u0441 u0435 u0431 u00a0缺相限制,在某一阶段内至少进行一次相邻点计算。21。 u043e u043f u0440 u0435 u0434 u0435 u043b u00a0 u0435 u043c u043e u0435 p.15的方法,其中 u043c u043e u043d u043e u0445 u0440 u0440 u043e u043c u04c u0430 u0442 u0438 u0447 u0435 u0441 u043a u043e u0435波场 u0432 u044b u0447 u0438 u0441 u043b u00a0 u044e u0442, u0438 u0441 u043f u043e u043b u044c u0443 u00a0至少一个功能绿色。; 22。第15页的方法,其中还包括 u0441 u0435 u0431 u00a0,根据 u0432 u044b u0447 u0438 u0441 u043b u0435 u043d u043d u043e u0433接收迁移的幅度系数 u043e u043c u043e u043d u043e u0445 u0440 u043e u043c u0430 u0442 u0438 u0447 u0435 u0441 u043a u043e u0433 u043e u043e u0432 u043e u043b u043d u043d laplacian u043f u043e u043b u00a0。; 23。 u043c u043e u043d u043e u0445 u0440 u043e u043c u0430 u0442 u0438 u0447 u0435 u0441 u043a u043e u0433 u043e p.15的确定方法,其中波动 u043f u043e u043b u00a0还包括 u0441 u0435 u0431 u00a0在多维表面上的波 u043f u043e u043b u00a0的计算。 u043c u043e u043d u043e u0445 u0440 u043e u043c u0430 u0442 u0438 u0447 u0435 u0441 u043a u043e u0433 u043e p.15的确定方法,其中波动 u043f u043e u043b u00a0进一步包括 u043f u043e u043e u043b u00b0在多维表面 u0440 u0430 u00a0 u043f u0440 u0435 u0434 u0441 u0442 u0430 u0432 u043b u00a0 u0435 u0442 a u0434 u0432 u0430 u0434 u0446 u0430 u0442 u0438 u0433 u0440 u0430 u043d u043d u043d u043d u0433 u043a。; 25。第15页的方法,其中 u043c u043e u043d u043e u0445 u0440 u043e u043c u0430 u0442 u0438 u0447 u0435 u0441 u043a u043e u043e u0433 u043e波动 u043f u043e u043b u00a0还包括 u0441 u0435 u0431 u00a0 u0440 u0435 u0448 u0435 u043d u0438 u00a0 u0434 u043b u00a0至少其中一项的计算:(i)波浪 u0443 u0440 u0430 u0432 u043d u0435 u043d u0438 u00a0弹性波 u0434 u043b u00a0沿一个方向传播,(ii)波 u0443 u0440 u0430 u0432 u043d u043d u0435 u043d u0438 u00a0弹性波 u0434 u043b u00a0总里程。(iii)声波 u0443 u0440 u0430 u0432 u043d u0435 u043d u0438 u00a0声波 u0434 u043b u00a0沿一个方向传播,并且(iv)声波 u0443 u0440 u0430 u0432 u043d u0435 u043d u0438 u00a0声波 u0434 u043b u00a0总里程。; 26。 u043c u043e u043d u043e u0445 u0440 u043e u043c u0430 u0442 u0438 u0447 u0435 u0441 u043a u043e u0433 u043e p.15的确定方法,其中波动 u043f u043e u043b u00a0还包括 u0441 u0435 u0431 u00a0进程 u0440 u0435 u0448 u0435 u043d u0438 u00a0 u0434 u043b u00a0 u043d u0430 u0445 u043e u0436 u0435 u043d u0438 u00a0解决方案 u0443 u0440 u0430 u0432 u043d u0435 u043d u0438 u00a0波动至少其中之一:(i)有限 u0440 u0430 u0437 u043d u043e u0441 u0442 u0435 u0439,(ii)有限元方法 u00a0 u0432 u043d u043e u0433 u043e,(iii),(iv)和(v) u043d u0435 u00a0 u0432 u043d u043e u0433 u043e方法 u043f u0440 u0435 u043e u0431 u0440 u0430 u0437 u043e u0432 u0430 u043d u0438 u00a0傅立叶方法。; 27。第15页的方法,其中至少要计算地震波的时间定义还包括 u0441 u0435 u0431 u00a0,其中至少一项是:(i)肛门isa局部梯度时间,(ii )分析局部梯度 u043d u0435 u0440 u0430 u0437 u0432 u0435 u0440 u043d u0443 u0442 u043e u0439相位,(iii) u043e u043f u0440 u04340 u0435 u0434 u0435 u043b u0435 u043d u0438 u00a0与计算相邻的至少一个最大振幅(iv)至少一个计算点的最小开相的定义,(v)平坦波 u0434 u043b 至少一个其他点的u00a0您是 u0447 u0438 u0441 u043b u0435 u043d u0438 u0439,(vi)加权平面波 u0434 u043b u00a0至少有一个相邻点计算,并且(vii)在至少一个相邻点计算上对 u0441 u043d u043e u0432 u0430 u043d u0438 u0438上的加权波脉冲 u0433 u044e u0439 u0433 u0435 u043d u0441 u0430的计算; 28。方法 u0434 u043b u00a0 u043e u043f u0440 u0435 u0434 u0435 u043b u0435 u043d u0438 u00a0在至少地质环境中可用的点 u0438 u00a0,包括 u0441 u0435 u0431 u00a0 :;(a)区域分配模型,包括地质环境中的许多点 u0441 u0435 u0431 u00a0 u0440 u0430 u0437 u043c u0435 u0449 u0435 u043d u043d u0438 u00a0;(b)计算波 u043f u043e至少使用一个快速模型 u0434 u043b u00a0计算至少一个选定频率中的至少一个选定频率。(c)在至少一个频率中定义地震波的开放相位。计算点,最接近指定 u0440 u0430 u0437 u043c u0435 u0449 u0435 u043d u0438 u00a0中至少一个点计算的点; (d)确定在定义的开放相位和 u0432 u044b u0447 u0438 u0441 u043b u0435 u043d u043d u043d u043e u043c u0443中至少计算一次地震波的时间 u0432 u043e u043b u043d u043e u0432 u043e u043c u0443字段 u0434 u043b u00a0至少计算一个点。29。第28页的方法,其中 u043f u0440 u0435 u0434 u0441 u0442 u0430 u0432 u043b u00a0 u0435 u0442的表面上的点为:(i) u043c u0435 u0441 u0442 u043e u043f u043e u043b u043e u0436 u0435 u043d u0438 u00a0源,以及(ii) u043c u0435 u0441 u0442 u043e u043f u043e u043e u043b u043e u0436 u0435 u043d u0438 u00a0接收器;; 30。第28页的方法,其中计算波 u043f u043e u043b u00a0 u0434 u043b u00a0至少进行一点计算还包括 u0441 u0435 u0431 u00a0 u0440 u0435 u0448 u0435 u043d u0438 u00a0 u043f u043e u043b u00a0向我挥舞以下至少一项的选定频率 u0434 u043b u00a0:(i)波浪 u0443 u0440 u0430 u0432 u043d u0435 u043d u0438 u00a0弹性波 u0434 u043b u00a0沿一个方向传播,(ii)波浪 u0443 u0440 u0430 u0432 u043d u0435 u043d u043d u0438 u00a0弹性波d u043b u00a0总行驶里程。(iii)波浪 u0443 u0440 u0430 u0432 u043d u0435 u043d u0438 u00a0声波 u0434 u043b u00a0沿一个方向传播,而(iv)波浪 u0443 u0440 u0430 u0432 u043d u0435 u043d u0438 u00a0声波 u0434 u043b u00a0总里程。; 31。第30页的计算 u043c u043e u043d u043e u0445 u0440 u043e u043c u0430 u0442 u0438 u0447 u0435 u0431 u043a u043e u0433 u043e第30页的方法u043b u00a0还包括 u0441 u0435 u0431 u00a0进程 u0440 u0435 u0448 u0435 u043d u0438 u00a0 u0434 u043b u00a0 u043d u0430 u0445 u04345 u043e u0436 u0434 043 u0438 u00a0解决方案 u0443 u0440 u0430 u0432 u043d u0435 u043d u0438 u00a0在以下至少一项上产生p波:(i)有限元方法,(ii)有限 u0440 u0430 u0437 u043d u043e u0441 u0442 u0435 u0439,(iii)和(iv) u00a0 u0432 u043d u043e u0433 u043e方法 u043d u0435 u00a0 u0432 u043d u043e u0433 u043e方法。; 32。计算波浪 u043f u043e u043b u00a0第30页的方法,其中还包括至少使用一个函数 u0441 u0435 u0431 u00a0绿色 u0434 u043b u00a0至少通过一次 u043d u043d u043e u0439频率;; 33。 p.30的方法,其中还包括 u0441 u0435 u0431 u00a0根据波 u043f u043e u043b u00a0 u0432 u044b u0447 u0438 u0441 u0431 u043b u0435 u043d la043d u043e u0433 u043e拉普拉斯语;; 34。 p.28的方法,其中至少一个点到许多点的计算包括计算。35。 p.28的方法,其中至少一个 u0441 u043e u0441 u0435 u0434 u043d u00a0 u00a0点计算包括 u0441 u0435 u0431 u00a0许多相邻点计算。第28页的方法,其中还包括基于至少一个 u0432 u044b u0447 u0438 u0441 u043b u0435 u043d u043d u043e u0433 u043e时间的 u0441 u0435 u0431 u00a0定义至少其中之一:(i)记录里程和(ii)距离表。; 37。第28页的方法,其中至少一个 u0441 u043e u0441 u0435 u0434 u043d u00a0 u00a0点计算包括 u0441 u0435 u0431 u00a0许多相邻点计算,并且该方法还包括 u0441 u0435 u0431 u00a0通过 u043e u0431 u0440 u0430 u0437 u043e u0432 u0430 u043d u0438 u00a0定义相邻点计算的相位的相加。 38。确定断相的方法,第28页,其中至少一个点计算包括 u0441 u0435 u0431 u00a0断相限制,在某一阶段内至少进行一次 u0447 u043a u0438计算 u0434 u043b u00a0至少计算一个相邻点; 39。 1的方​​法,其中时间的定义还包括 u0441 u0435 u0431 u00a0波浪 u043f u043e u043b u00a0 u0434 u043b u00a0计算至少在 u043c u043d 中选择的频率之一40。 1的方​​法,其中时间的定义还包括 u0441 u0435 u0431 u00a0 wave u043f u043e u043b u00a0 u0434 u043b u00a0计算 u043c u043d u043e u0433中至少一个所选频率 u043e u0433 ranna surface u043a u043e u0442 u043e u0440 u0430 u00a0 u043f u0440 u0435 u0434 u0441 u0442 u0430 u0432 u043b u043b u00a0 u0435 u0442 a u0434 u0432 u0430 u0434 u0446 u0430 u0442 u0438 u0433 u0440 u0430 u043d u043d u0438 u043a.41。第15页的方法,其中至少要计算地震波的时间定义还包括 u0441 u0435 u0431 u00a0,其中至少一项是:(i)肛门isa局部梯度时间,(ii )分析局部梯度 u043d u0435 u0440 u0430 u0437 u0432 u0435 u0440 u043d u0443 u0442 u043e u0439相位,(iii) u043e u043f u0440 u04340 u0435 u0434 u0435 u043b u0435 u043d u0438 u00a0与计算相邻的至少一个最大振幅(iv)至少一个计算点的最小开相的定义,(v)平坦波 u0434 u043b 至少一个其他点的u00a0您是 u0447 u0438 u0441 u043b u0435 u043d u0438 u0439,(vi)加权平面波 u0434 u043b u00a0至少有一个相邻点计算,并且(vii)在至少一个相邻点计算上,对 u0441 u043d u043e u0432 u0430 u043d u0438 u0438上的加权波脉冲 u0433 u044e u0439 u0433 u0435 u043d u0441 u0430进行计算。

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