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    • 4. 发明授权
    • Design of reconnaissance surveys using controlled source electromagnetic fields via probabilistic neural network
    • 通过概率神经网络设计使用受控源电磁场的侦察调查
    • US07792766B2
    • 2010-09-07
    • US11886171
    • 2006-03-20
    • Richard T. HouckDmitriy Pavlov
    • Richard T. HouckDmitriy Pavlov
    • G06F19/00G06F17/00G06G7/48H04H9/00
    • G01V3/083
    • Method for determining an expected value for a proposed reconnaissance electromagnetic (or any other type of geophysical) survey using a user-controlled source. The method requires only available geologic and economic information about the survey region. A series of calibration surveys are simulated with an assortment of resistive targets consistent with the known information. The calibration surveys are used to train pattern recognition software to assess the economic potential from anomalous resistivity maps. The calibrated classifier is then used on further simulated surveys of the area to generate probabilities that can be used in Value of Information theory to predict an expected value of a survey of the same design as the simulated surveys. The calibrated classifier technique can also be used to interpret actual CSEM survey results for economic potential.
    • 使用用户控制源确定拟议侦察电磁(或任何其他类型的地球物理)勘测的预期值的方法。 该方法只需要有关调查区域的可用的地质和经济信息。 使用与已知信息一致的各种电阻目标模拟一系列校准调查。 校准调查用于训练模式识别软件,以评估异常电阻率图的经济潜力。 然后将校准的分类器用于对该区域的进一步模拟调查,以产生可用于信息价值理论的概率,以预测与模拟调查相同设计的调查的预期值。 校准分类技术也可用于解释实际的CSEM调查结果的经济潜力。
    • 6. 发明授权
    • Shaped high frequency vibratory source
    • 形高频振动源
    • US07436734B2
    • 2008-10-14
    • US10550406
    • 2004-02-13
    • Christine E. Krohn
    • Christine E. Krohn
    • G01V1/00G01V1/155
    • G01V1/005G01V1/368G01V1/37
    • The present invention is a method of processing seismic data in which one or more seismic vibrators are activated with one or more pilot signals and vibrator motions are recorded along with seismic data. Vibrator signatures are computed from measured vibrator motions, such as the ground force signal. A desired impulse response is specified from either a measured vibrator motion or from test data or field data from a location near the location from which the seismic data was acquired. A deconvolution filter is computed from the impulse response and the vibrator signature. Alternatively, a single separation and deconvolution filter is derived from the impulse response and from vibrator signatures from multiple vibrators and sweeps. The deconvolution or deconvolution and separation filter is used to process the seismic data. The vibrators are then moved to a new location, and the activation is repeated.
    • 本发明是一种处理地震数据的方法,其中一个或多个地震振动器由一个或多个导频信号激活,振动器运动与地震数据一起被记录。 振动器特征由测量的振动器运动计算,如地面力信号。 从测量的振动器运动或来自测量数据或来自获取地震数据的位置附近的位置的场数据指定期望的脉冲响应。 根据脉冲响应和振动器签名计算去卷积滤波器。 或者,单个分离和去卷积滤波器来自脉冲响应和来自多个振动器和扫描的振动器特征。 去卷积或去卷积和分离滤波器用于处理地震数据。 然后将振动器移动到新位置,并重复激活。
    • 7. 发明授权
    • Method for obtaining porosity and shale volume from seismic data
    • 从地震数据中获取孔隙度和页岩体积的方法
    • US08126651B2
    • 2012-02-28
    • US11922815
    • 2006-06-06
    • Rebecca L. SaltzerChristopher J. FinnRongrong Lu
    • Rebecca L. SaltzerChristopher J. FinnRongrong Lu
    • G01V1/00G01V1/28
    • G01V1/306
    • Method for obtaining rock parameters such as porosity and vshale directly from inversion of seismic data corresponding to a single trace location. This method is distinguished from existing methods that obtain elastic properties from inversion of seismic data, then relate the elastic parameters to rock lithology parameters such as porosity or vshale because it is accomplished in one step, can incorporate anisotropy and does not require multiple trace locations for stability. The data are separated into partial stacks, and a wavelet is specified for each stack. A set of linearized equations are constructed relating seismic reflectivity to changes in elastic parameters, and another set of linearized equations is constructed relating the changes in elastic parameters to the lithologic parameters. The linearized reflectivity equations are combined with the linearized rock physics equations, convolved with the specified wavelets, and equated to the seismic data. The resulting matrix equations are then inverted and a solution is obtained for all offsets simultaneously.
    • 直接从对应于单一轨迹位置的地震数据反演获得岩石参数如孔隙度和垂直叶片的方法。 该方法与从地震数据反演获得弹性性质的现有方法不同,然后将弹性参数与岩石岩性参数(如孔隙度或vshale)相关联,因为它在一个步骤中完成,可以包含各向异性,并且不需要多个迹线位置 稳定性。 数据被分成部分堆栈,并为每个堆栈指定一个小波。 构造了一组线性方程,将地震反射率与弹性参数的变化相关联,另外建立了一组线性化方程,将弹性参数的变化与岩性参数相关联。 线性化反射率方程与线性化岩石物理方程组合,与指定的小波卷积,并等同于地震数据。 然后将所得到的矩阵方程反相,同时获得所有偏移的解。
    • 9. 发明授权
    • Method for correcting the phase of electromagnetic data
    • 电磁数据相位校正方法
    • US08121789B2
    • 2012-02-21
    • US12303673
    • 2007-06-12
    • Thomas A. DickensCharlie JingDennis E. Willen
    • Thomas A. DickensCharlie JingDennis E. Willen
    • G01V1/40
    • G01V3/12G01V3/083
    • Method for identifying, determining and correcting source-related phase errors in data from a controlled source electromagnetic survey by using data from ordinary survey receivers, i.e. without benefit of source monitoring data. Abrupt anomalies indicating source malfunctions are identified (71) in the time domain by plotting time intervals between neighboring zero crossings or by zero-lag cross correlation between consecutive bins of receiver data, and the amount of the time error (73) can be determined by performing cross correlation between two bins on either side of an anomaly. In the frequency domain, transmitter anomalies can be identified by looking for discontinuities in plots of phase vs. offset, and the corrective phase shift can be determined by matching the phase on one side of the anomaly to that on the other side. A global time/phase shift (76) can be determined by using phase frequency-scaling behavior at near offsets.
    • 用于通过使用普通测量接收机的数据来识别,确定和校正来自受控源电磁勘测的源相关相位误差的方法,即不受源监测数据的益处。 在时域中通过绘制相邻过零点之间的时间间隔或接收器数据的连续箱之间的零时相互相关来识别(71)在时域中的突发异常,并且时间误差量(73)可以由 在异常的任一侧执行两个箱之间的互相关。 在频域中,可以通过查找相位偏移图中的不连续性来识别发射机异常,并且可以通过将异常一侧的相位与另一侧的相位匹配来确定校正相移。 全局时间/相移(76)可以通过使用接近偏移的相位频率缩放行为来确定。