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    • 3. 发明申请
    • METHOD OF AND APPARATUS FOR EXPLORING A REGION BELOW A SURFACE OF THE EARTH
    • 用于探索地球表面以下地区的方法和装置
    • WO2009081150A1
    • 2009-07-02
    • PCT/GB2008/004243
    • 2008-12-22
    • STATOILHYDRO ASAROBINSON, JohnBUSSAT, SaschaHANSSEN, PeterKUGLER, Simone
    • BUSSAT, SaschaHANSSEN, PeterKUGLER, Simone
    • G01V1/00
    • G01V1/28G01V1/30G01V2210/1236
    • A passive method is provided for exploring a region below the surface of the earth. The method comprises using a single sensor located in turn at a plurality of locations to obtain seismic data obtained by recording ambient seismic interface waves in a frequency range whose lower limit is greater than OHz, and whose upper limit is less than or equal to substantially 1 Hz. The data are processed (41-44) so as to obtain a measure of the energy in a frequency band within the frequency range. For example, the seismic data may be filtered (41 ) and may be subjected to amplitude normalisation (42) before being transformed (43) into the frequency domain. The energy measure may then be calculated (44) by integrating the spectrum in the frequency domain over a desired frequency range. The resulting calculated energy provides information about the region of the earth being explored.
    • 提供了一种无源方法来探索地球表面以下的区域。 该方法包括使用依次位于多个位置的单个传感器,以获得通过在下限大于OHz的频率范围内记录环境地震界面波而获得的地震数据,并且其上限小于或等于基本上为1 赫兹。 处理数据(41-44),以获得在频率范围内的频带中的能量的量度。 例如,地震数据可以被滤波(41),并且可以在变换(43)到频域之前进行幅度归一化(42)。 然后可以通过在频域中在所需频率范围内积分频谱来计算能量测量(44)。 所得到的计算能量提供了有关正在探索的地球区域的信息。
    • 4. 发明申请
    • METHOD OF AND APPARATUS FOR EXPLORING A REGION BELOW A SURFACE OF THE EARTH
    • 用于探索地球表面以下地区的方法和装置
    • WO2009081210A1
    • 2009-07-02
    • PCT/GB2008/051223
    • 2008-12-22
    • STATOILHYDRO ASAROBINSON, JohnBUSSAT, SaschaHANSSEN, PeterKUGLER, Simone
    • BUSSAT, SaschaHANSSEN, PeterKUGLER, Simone
    • G01V1/00
    • G01V1/28G01V1/30G01V2210/1236
    • A passive method is provided for exploring a region below the surface of the earth. The method comprises using a plurality of sensors (20, 21) to obtain seismic data obtained by recording ambient seismic interface waves in a frequency range whose lower limit is greater than 0Hz, and whose upper limit is less than or equal to substantially 1Hz. The sensors (20, 21) may be sensitive to three orthogonal components. Recordings may be made simultaneously by all sensors (20, 21) and normalisation of data is unnecessary. The sensors (20, 21) may be moved and clean data may be selected. Local dispersion curves may be determined to improve vertical resolution. The data are processed (41-44) so as to obtain a measure of the energy in a frequency band within the frequency range. The energy measure may be calculated (44) by integrating the spectrum in the frequency domain over a desired frequency range. The resulting calculated energy provides information about the region of the earth being explored.
    • 提供了一种无源方法来探索地球表面以下的区域。 该方法包括使用多个传感器(20,21)来获取通过在下限大于0Hz并且其上限小于或等于大致1Hz的频率范围内记录环境地震界面波而获得的地震数据。 传感器(20,21)可能对三个正交分量敏感。 记录可以由所有传感器(20,21)同时进行,并且数据的标准化是不必要的。 可以移动传感器(20,21),并且可以选择清洁数据。 可以确定局部色散曲线以改善垂直分辨率。 处理数据(41-44),以获得在频率范围内的频带中的能量的量度。 可以通过在频域中在所需频率范围内积分频谱来计算能量测量(44)。 所得到的计算能量提供了有关正在探索的地球区域的信息。