The influence of mesoscopic flow on the P-wave attenuation and dispersion in a porous media permeated by aligned fractures /
a1_In sedimentary rocks attenuation/dispersion is dominated by fluid-rock interactions. Wave-induced fluid flow in the pores causes energy loss through several mechanisms, and as a result attenuation is strongly frequency dependent. However, the fluid motion process governing the frequency dependent...
Další autoři: |
Deng, Jixin
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Autor )
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Typ dokumentu: | Článek |
Jazyk: |
angličtina |
ISSN: | 0039-3169 |
Zdroj: | Studia geophysica et geodaetica: Vol. 57, č.3 (2013), s. 482-506. |
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