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Titlebook: Velocities in Reflection Seismology; Jean-Pierre Cordier Book 1985 Springer Science+Business Media B.V. 1985 Borehole.formation.prospectin

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書目名稱Velocities in Reflection Seismology
編輯Jean-Pierre Cordier
視頻videohttp://file.papertrans.cn/981/980992/980992.mp4
叢書名稱Modern Approaches in Geophysics
圖書封面Titlebook: Velocities in Reflection Seismology;  Jean-Pierre Cordier Book 1985 Springer Science+Business Media B.V. 1985 Borehole.formation.prospectin
描述Although considera bIe efforts are now being made to find new sources of energy, alI the experts are agreed that hydrocarbons will have to provide the greater part of our energy needs for a generation ahead. Exploration for and production of hydrocarbons therefore pose a serious problem for our future, as much for the quantitative satisfaction of our requirements as for our search for self-sufficiency in energy. As a direct result of improvements in technology throughout the world, geophysics has progressively enlarged its field of influence in the realms of exploration and production. But amongst the various geophysical methods available, seismic reflection has gradually become accepted as the basic tool of the oiI prospector. Reflection seismology has reached and consolidated this position because it has shown itself to be capable of adapting to the increasing complexity of the requirements of exploration. Initially directed towards geometric mapping of the sub-surface, it became the means of detection of structural traps in geotectonically quiescent regions, and thereafter in increasingly complex surroundings. It has enabled us to clothe the structural framework with a lithology
出版日期Book 1985
關(guān)鍵詞Borehole; formation; prospecting; seismic; seismology; economic geology
版次1
doihttps://doi.org/10.1007/978-94-017-3641-1
isbn_softcover978-90-481-8416-3
isbn_ebook978-94-017-3641-1Series ISSN 0924-6096
issn_series 0924-6096
copyrightSpringer Science+Business Media B.V. 1985
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Calculation of Interval Velocities,e the velocities in the layers, using DIX’s formula (which follows directly from the definition of V.): . where .. = velocity measured at time t.; V. = velocity measured at time t.; V. = velocity of the layer of material included between times t. and t..
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978-90-481-8416-3Springer Science+Business Media B.V. 1985
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Basic Ideas on the Propagation of Seismic Waves,The object of this short chapter is to give a simple account of the definitions and basic concepts which are essential for an understanding of the following chapters.
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Velocities in Seismic Reflection. Definitions. Principles of Velocity Analysis,The problem of velocities in seismic reflection affects two essential aspects of the work of the interpreter:
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