西南石油大学学报(自然科学版) ›› 2010, Vol. 32 ›› Issue (2): 53-57.DOI: 10.3863/j.issn.1674-
• 地质勘探 • Previous Articles Next Articles
MEI Sheng-quan,ZHONG Ben-shan
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Abstract:
The two-point ray-tracing is an effective method to solve complex geological structure reflection wave ray-tracing.In this paper,a new two-point ray-tracing method is proposed,it is based on the first-break wave ray-tracing tomography algorithm,and grid division is used to discrete model,through the forward procession of two-step ray-tracing method,the grid cells minimum travel-time from source point and receive point is calculated respectively,and each cell sum of the twice travel-times is taken as the minimum travel-time,again along the layer interface,the nearest minimum travel-time cell is researched.Then the Particle Swarm Optimization (PSO) algorithm is used to search the minimum travel-time point in this cell,as the reflex point,through the backward procession,the ray path is traced from this point to source point and receive point respectively with the Linear Travel-time Interpolation (LTI) algorithm.Finally the two-point ray-tracing path is obtained.
Key words: linear travel-time interpolation algorithm, grid division, two-point ray-tracing, preliminary wave, seismic survey
CLC Number:
TE132.1
P631.4
MEI Sheng-quan;ZHONG Ben-shan. A TWO-POINT RAY-TRACING METHOD BASED ON GRID-DIVISION[J]. 西南石油大学学报(自然科学版), 2010, 32(2): 53-57.
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URL: http://journal15.magtechjournal.com/Jwk_xnzk/EN/10.3863/j.issn.1674-
http://journal15.magtechjournal.com/Jwk_xnzk/EN/Y2010/V32/I2/53