Titlebook: Seismic Reflection Processing; With Special Referen S. K. Upadhyay Textbook 2004 Springer-Verlag Berlin Heidelberg 2004 Anisotropy.Earth Re

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書目名稱Seismic Reflection Processing影響因子(影響力)




書目名稱Seismic Reflection Processing影響因子(影響力)學(xué)科排名




書目名稱Seismic Reflection Processing網(wǎng)絡(luò)公開度




書目名稱Seismic Reflection Processing網(wǎng)絡(luò)公開度學(xué)科排名




書目名稱Seismic Reflection Processing被引頻次




書目名稱Seismic Reflection Processing被引頻次學(xué)科排名




書目名稱Seismic Reflection Processing年度引用




書目名稱Seismic Reflection Processing年度引用學(xué)科排名




書目名稱Seismic Reflection Processing讀者反饋




書目名稱Seismic Reflection Processing讀者反饋學(xué)科排名

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Reflection Time Analysis and Velocities for Transversely Isotropic (T. I.) Media,In Chapter 7, various velocity terms relevant to the analysis of a layered isotropic medium were explained. It was shown that surface seismic reflection data could be utilized to find an interval property (velocity) of the subsurface medium.

Paradox

Panther

S. K. UpadhyayShows most recent developments in anisotropy.Contains well-illustrated diagrams as well as exercises with solutions

誘騙

978-3-642-07414-1Springer-Verlag Berlin Heidelberg 2004

Lobotomy

Reflection Data Acquisition, land or sea), depth to be probed, and inhabitance, etc. Commonly used seismic sources in land areas are explosives, except in populated areas with a large density of dwellings. For seismic surveys in marine areas, a source like ‘sparker’ or ‘a(chǎn)ir-gun’ is used.

eustachian-tube

Attributes of Routine Reflection Processing and Pitfalls,ot only precise structural interpretations are possible but valuable conclusions may be deduced about lithology, fluid content, porosity, stratification, depositional processes and environments, sediment transport direction and geological evolution, etc.

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calumniate

Reflection Time Analysis and Velocity for Isotropic Layered Media, of realistic velocity estimation owes its complexity to heterogeneity of the subsurface and the lack of knowledge of seismic ray paths. For a heterogeneous ground, the ray path deviates from a straight line. In fact, the ray path is the least time path (.). According to Fermat’s principle: ..

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