首頁(yè) 資料分類 用戶榜 | 積分說(shuō)明    

      ·Moveout-based geometrical-spreading correction


    資料星級(jí): 資料格式:pdf
    上 傳 者:zhaoweiping 下載次數(shù):2
    上傳時(shí)間:2010-01-14 11:57:56

    1分
    546KB
    收藏  舉報(bào)     發(fā)送給好友

      詳細(xì)介紹: 發(fā)表評(píng)論   
    Moveout-based geometrical-spreading correction for converted waves

    Geometrical-spreading correction is an important component of amplitude-
    variation-with-offset (AVO) analysis, which provides high-resolution informa-
    tion for anisotropic parameter estimation and fracture characterization. Here,
    we extend the algorithm of moveout-based anisotropic spreading correction
    (MASC) to mode-converted PSV-waves in VTI (transversely isotropic with a
    vertical symmetry axis) media and symmetry planes of orthorhombic media.
    While the geometrical-spreading equation in terms of reflection traveltime has
    the same form for all wave modes in laterally homogeneous media, reflection
    moveout of PS-waves is more complicated than that of P-waves (e.g., it can be-
    come asymmetric in common-midpoint geometry). Still, for models with a hor-
    izontal symmetry plane, long-spread reflection traveltimes of PS-waves can be
    well-approximated by the Tsvankin-Thomsen and Alkhalifah-Tsvankin move-
    out equations, which are widely used for P-waves. Although the accuracy of
    the Alkhalifah-Tsvankin equation is somewhat lower, it includes less moveout
    parameters and helps to maintain the uniformity of the MASC algorithm for P-
    and PS-waves. The parameters of both moveout equations are obtained by least-
    squares traveltime fitting or semblance analysis and are different from those for
    P-waves.
    Testing on full-wavefield synthetic data generated by the reflectivity method for
    layered VTI media confirms that MASC accurately reconstructs the plane-wave
    conversion coefficient from conventional-spread PS data. Errors in the estimated
    conversion coefficient, which become noticeable at moderate and large offsets,
    are mostly caused by offset-dependent transmission loss of PS-waves.
      該用戶還有這些資料: 更多   

    應(yīng)用地震多屬性反演與隨機(jī)模擬技術(shù)_省略...

    準(zhǔn)噶爾盆地西北緣辮狀河沉積模式探_省略...

    北部上侏羅統(tǒng)辮狀河體系沉積特征_郭佳

    坳陷湖盆斜坡帶辮狀河砂體分布與有_省略...

    碳酸鹽巖儲(chǔ)層地震信息響應(yīng)及橫向預(yù)測(cè)

    如何提高產(chǎn)層深度預(yù)測(cè)的準(zhǔn)確度

    全數(shù)字地震疊前彈性交會(huì)技術(shù)及應(yīng)用

    強(qiáng)屏蔽層下弱反射儲(chǔ)層特征分析及識(shí)別方法

    利用地震信息評(píng)價(jià)陸相盆地巖性圈閉的關(guān)鍵...


     
      其他相關(guān)資料: 更多   

    Technicial English

    permian basin oil a...

    2014 USA Lorado llc

    韓國(guó)OSCG電纜密封接頭樣本

    NACE MR0175 ISO 151...

    斯倫貝謝 AMOCO最全的固控資料 P...

    201310三維保幅彎曲射線Kirch...

    201310彈性波Kirchhoff疊...

    201309基于Kirchhoff偏移...



    国产人妻人伦精品1国产盗摄 | 精品视频一区二区三区| 国产精品色午夜免费视频| 精品久久久久久蜜臂a∨| 奇米影视7777久久精品| 精品久久久久久亚洲| 国产午夜精品久久久久九九电影 | 国产成人精品日本亚洲网站 | 少妇人妻偷人精品视频| 亚洲韩国精品无码一区二区三区| 国产精品国产三级国产潘金莲| 嘿嘿射久草日韩视频| 日韩精品中文字幕视频一区 | 亚洲日韩国产精品乱| 无码日韩AV一区二区三区| 国产精品亚洲精品日韩已满| 国产精品jvid在线观看| 精品一区二区久久久久久久网精| 十八禁无遮挡99精品国产| 99爱在线精品免费观看| 国产cosplay精品视频| 中文字幕亚洲精品资源网| 99热这里只有精品99| 人妻少妇精品视频二区 | 日韩精品无码免费专区网站 | 久久精品国产2020观看福利| 成人午夜精品无码区久久| 日本无码小泬粉嫩精品图| 99re6在线精品免费观看| 久久综合精品国产一区二区三区 | 伊人久久精品无码二区麻豆| 日韩人妻无码精品系列| 中文国产成人精品久久久| 久久久精品国产亚洲成人满18免费网站| 国产精品婷婷午夜在线观看 | 国产成人综合一区精品| 日产精品一卡2卡三卡4乱码| 99亚洲精品卡2卡三卡4卡2卡| 大伊香蕉在线精品视频人碰人| 日本精品在线观看视频| 国产精品亚洲专区在线播放|