seismic anisotropy 中文意思是什麼

seismic anisotropy 解釋
地震各向異性現象
  • seismic : adj 地震（性）的；由地震引起的；易生地震的。 a seismic area 震域；震區。 the seismic centre [focu...
  • anisotropy : 彈性導向性
  1. Ming, h. y. and li, x. s. ( 2007 ). " numerical study of impact of soil anisotropy on seismic performance of retaining structure. " international journal of geomechanics, asce, 7 ( 5 ). in press

    明海燕，李相崧（ 2007 ） . "砂土各向異性對擋土墻抗震性能影響數值分析. "深圳大學學報理工版，第24卷，第3期，出版中
  2. Lattice preffered orientation and seismic anisotropy of ultramafic xenoliths in damaping, hebei province

    河北大麻坪超基性巖包體的巖石組構和地震波速各向異性
  3. Conventional seismic data processing method uses hyperbolic equation to describe time - distance formula of reflection wave, error of this equation increases with the increase of heterogeneity, anisotropy and spread length

    常規地震資料處理方法是利用雙曲線方程來描述反射波時距曲線規律，此方程隨著地層非均質性、各向異性和排列長度的增加，其誤差變大。
  4. Lattice preferred orientation ; seismic anisotropy ; damaping

    晶格優選方位波速各向異性大麻坪
  5. Ava analysis plays an important role in the multiwave seismic data processing. the anisotropy, however, has an important influence on the ava. therefore, the multiwave amplitude characteristic equation of the anisotropic media should be established and then the ava analysis and parameter inversion could be realized

    Ava （ amplitudeversusangle -振幅隨入射角變化）分析在多波資料處理中有著重要的作用，然而介質各向異性對ava有著重要的影響，因此需要建立各向異性介質中的多波振幅特徵方程，以利於多波資料進行ava分析和地層參數反演。
  6. Directions are obtained by two means : calculation and measure. our investigations are summed as follows : 1 the lpo relations between olivine and orthopyroxene are different from usually situations : 100ol 001opx, 010ol 100opx, 001ol 010opx ; 2 the seismic anisotropy of the ultramafic rocks in damaping is obvious. their characters are consistent with the structures of the rocks and fabrics of minerals, which means seismic anisotropy is mainly controlled by rocks fabrics ; 3 seismic velocities suggest that the composition of upper mantle in damaping region is resemble to the xenoliths, which major component is lherzolite

    不同2大麻坪地區幔源包體的波速各向異性顯著，巖石的波速各向異性特徵與其宏觀構造和微觀組構一致，說明巖石組構是造成地震波速各向異性的決定因素3由地震波速推測的大麻坪地區的上地幔成分與包體出露的情況一致，即主體為二輝橄欖巖。
  7. In this paper, some key notes were introduced, such as 3 - component receiver, the designation of measuring system, processing modules based on seismic anisotropy, and joint process and interpretation of the seismic data

    為此，本文針對多分量數據採集、處理、解釋過程中的三分量檢波器、觀測系統設計、各向異性處理方法和處理解釋一體化進行了探討。
  8. Applied seismic forward modeling part : quantitative determination of thin layer anisotropy by pre - stack seismic forward modeling

    用地震正演疊前炮集記錄模擬方法定量解釋薄砂巖的各向異性
  9. A preliminary discussion on the application of multiwave seismic data to the study of anisotropy of various formations

    多波地震地層各向異性的初步研究和探討
  10. To explore the complex oil and gas reservoir, multi - component seismic technique, based on the theory of seismic anisotropy, has been applied a lot to some extend

    摘要基於地震各向異性理論的多分量地震勘探技術已得到一定程度的應用，以解決復雜油氣藏的勘探問題。
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