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    • 2. 发明授权
    • 3-D multiple attenuation
    • 3-D多重衰减
    • US5729506A
    • 1998-03-17
    • US751640
    • 1996-11-18
    • William Henry Dragoset, Jr.Louis Joseph Ward
    • William Henry Dragoset, Jr.Louis Joseph Ward
    • G01V1/36G01V1/38
    • G01V1/364G01V2210/56
    • A computationally economical method for applying multi-dimensional multiple-reflection attenuation to a marine seismic-signal data set comprised of a plurality of common shot gathers that have surface-multiple wavefields embedded therein. The multi-dimensional data are assumed to have been gathered from a plurality of parallel 2-D lines of survey. From every nth reference line, where n is a small number greater than 2, a common shot gather is selected. For every so-selected common shot gather, a reference surface-multiple wavefield is predicted as a function of offset and travel time with the aid of any well-known multiple attenuation routine, using a wavelet having fixed attributes in terms of amplitude, phase and frequency. A common shot gather is chosen from among the plurality of common shot gathers. The predicted surface-multiple wavefield nearest to the chosen common shot gather is adaptively filtered to match the predicted surface-multiple wavefield to the surface-multiple wavefield embedded in the chosen common shot gather. The matched predicted surface multiple wavefield is subtracted from the embedded surface multiple wavefield to provide a multiple-free common shot gather.
    • 一种用于将多维多重反射衰减应用于包含嵌入其中的表面多波场的多个共同射击集合的海洋地震信号数据集的计算经济方法。 假设多维数据已经从多个平行的2-D线调查中收集。 从第n个参考线,其中n是大于2的小数,选择一个共同的拍摄集合。 对于每个所选择的共同拍摄集合,借助于任何公知的多重衰减程序,使用在幅度,相位和相位上具有固定属性的小波,将参考表面多波场作为偏移和行进时间的函数预测 频率。 从多个共同的拍摄集合中选择共同的拍摄集合。 预测的表面多波场最接近所选择的共同点集合被自适应滤波,以将预测的表面多波场与嵌入所选共同射击集合中的表面多波场相匹配。 从嵌入式表面多波场中减去匹配的预测表面多波场,以提供多次共同的射击聚集。
    • 3. 发明授权
    • Dual-wavefield multiple attenuation
    • 双波场多重衰减
    • US08077544B2
    • 2011-12-13
    • US12058312
    • 2008-03-28
    • William Henry Dragoset, Jr.
    • William Henry Dragoset, Jr.
    • G01V1/38
    • G01V1/36G01V2210/56
    • Method for attenuating surface multiple reflections in dual-wavefield seismic data. In one implementation, the method may include: (a) performing wavefield separation on dual-wavefield seismic data to separate events in the seismic data into data sets according to ghost characteristics; (b) applying a multidimensional Surface-Related Multiple Elimination (SRME) to two or more of the data sets to yield an SRME result in a manner that retains surface reflection information affecting surface multiple reflections; and (c) repeating step (b) one or more times.
    • 双波场地震数据衰减表面多重反射的方法。 在一个实现中,该方法可以包括:(a)在双波场地震数据上执行波场分离,以根据鬼特征将地震数据中的事件分为数据集; (b)将多维表面相关多重消除(SRME)应用于两个或多个数据集,以产生影响表面多次反射的表面反射信息的方式产生SRME结果; 和(c)重复步骤(b)一次或多次。
    • 5. 发明授权
    • Method of predicting kinematics for surface multiples
    • 预测表面倍数运动学的方法
    • US06169959A
    • 2001-01-02
    • US09320954
    • 1999-05-27
    • William Henry Dragoset Jr.
    • William Henry Dragoset Jr.
    • G01V128
    • G01V1/36G01V2210/56
    • Traveltimes of multiply reflected seismic events in a seismic profile or a model are determined from traveltimes for primary events. The traveltimes for the primary events may be obtained by ray tracing through a velocity model of the subsurface of by picking traveltimes from primary reflection horizons present in an actual seismic data set. The traveltimes for the primary events define a traveltime table for various combinations of source and receiver locations. The traveltime for a multiple corresponding to specified source and receiver positions is then determined by summing the traveltimes for primary events from the source to an interim point and from the interim point to the receiver: the correct location of the interim point corresponding to an actual multiple reflection raypath from the source to the receiver is the one that, according to Fermat's principle, has the minimum value for the sum. This method is applicable to all primary events, so that subsurface multiples as well as water bottom multiples can be determined. The method may also be used for determining traveltimes for higher order multiples.
    • 地震剖面或模型中乘法反映的地震事件的旅行时间由主要事件的旅行时间确定。 主要事件的旅行时间可以通过通过从实际地震数据集中存在的主要反射视野拾取旅行时间的地下速度模型进行射线追踪来获得。 主要事件的旅行时间定义了源和接收器位置的各种组合的旅行时间表。 然后,通过将从源到临时点和从临时点到接收者的主要事件的行进时间相加来确定对应于指定的源和接收器位置的多个移动时间:对应于实际倍数的中间点的正确位置 从源到接收机的反射射线路径是根据费马原理,具有总和的最小值。 该方法适用于所有主要事件,从而可以确定地下倍数以及水底倍数。 该方法还可用于确定较高阶乘数。