物探与化探
物探與化探
물탐여화탐
GEOPHYSICAL AND GEOCHEMICAL EXPLORATION
2015年
1期
196-202
,共7页
任丽娟%李振春%王延光%刘兴达%孙小东
任麗娟%李振春%王延光%劉興達%孫小東
임려연%리진춘%왕연광%류흥체%손소동
各向异性%矢量波场%逆时偏移%数据分解
各嚮異性%矢量波場%逆時偏移%數據分解
각향이성%시량파장%역시편이%수거분해
anisotropy%vector wavefield%reverse time migration%data decomposition
基于两步法分离各向异性矢量波波场,第一步,将各向异性波动方程进行相似变换(使其具有明确直观的运动学和动力学特征),使其投影在各向同性方向上;第二步,各向异性介质传播算子波场分离基础上的波形校正,将投影于各向同性方向上的波场校正回各向异性方向上,最终达到各向异性波场分离的结果。笔者首先对VTI介质进行试算,以证明其可行性;此外,将地表数据进行分解,即所采集到的多分量地震数据在进行偏移成像之前先进行数据分解,得到纯净的qP波数据、qSV波数据以及qSH波数据,通过地表数据的分解将成像过程变成一个可控过程,通过对地表数据输入的控制得到我们所希望的成像结果分量,可以减少无谓的计算;对Hess模型正演炮记录进行了数据分解,并对其进行了逆时偏移成像以验证理论的可行性。
基于兩步法分離各嚮異性矢量波波場,第一步,將各嚮異性波動方程進行相似變換(使其具有明確直觀的運動學和動力學特徵),使其投影在各嚮同性方嚮上;第二步,各嚮異性介質傳播算子波場分離基礎上的波形校正,將投影于各嚮同性方嚮上的波場校正迴各嚮異性方嚮上,最終達到各嚮異性波場分離的結果。筆者首先對VTI介質進行試算,以證明其可行性;此外,將地錶數據進行分解,即所採集到的多分量地震數據在進行偏移成像之前先進行數據分解,得到純淨的qP波數據、qSV波數據以及qSH波數據,通過地錶數據的分解將成像過程變成一箇可控過程,通過對地錶數據輸入的控製得到我們所希望的成像結果分量,可以減少無謂的計算;對Hess模型正縯砲記錄進行瞭數據分解,併對其進行瞭逆時偏移成像以驗證理論的可行性。
기우량보법분리각향이성시량파파장,제일보,장각향이성파동방정진행상사변환(사기구유명학직관적운동학화동역학특정),사기투영재각향동성방향상;제이보,각향이성개질전파산자파장분리기출상적파형교정,장투영우각향동성방향상적파장교정회각향이성방향상,최종체도각향이성파장분리적결과。필자수선대VTI개질진행시산,이증명기가행성;차외,장지표수거진행분해,즉소채집도적다분량지진수거재진행편이성상지전선진행수거분해,득도순정적qP파수거、qSV파수거이급qSH파수거,통과지표수거적분해장성상과정변성일개가공과정,통과대지표수거수입적공제득도아문소희망적성상결과분량,가이감소무위적계산;대Hess모형정연포기록진행료수거분해,병대기진행료역시편이성상이험증이론적가행성。
Two?step separation was conducted for anisotropy vector wavefield.The first step is to make the anisotropic elastic wave equa?tion in the polarization direction of the projection isotropic so that it has clear and intuitive kinematic and dynamic characteristics;the second step is to calculate anisotropic medium propagator wavefield separation waveform correction based on the correction of the projec?ted direction of the wavefield in the isotropic direction back to the anisotropic direction, and ultimately the anisotropic wavefield separa?tion can be achieved.First of all,the test of VTI media proves its feasibility.In addition,the authors put forward the surface data decom?position,namely,data decomposition is conducted for collected multicomponent seismic data before the migration imaging.In order to get the pure qP wave,qSH wave and qSV wave data the authors conducted the surface data input control to obtain the satisfactory imaging results of components and make imaging decomposition of the surface data performed in a controlled process,thus reducing unnecessary computation.The authors conducted decomposition of Hess forward modeling shot record data and reverse?time migration imaging.