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    • 4. 发明申请
    • Seismic Horizon Skeletonization
    • 地震地震骨骼化
    • US20130151161A1
    • 2013-06-13
    • US13757466
    • 2013-02-01
    • Matthias G. ImhofDominique G. GillardStefan HussenoederPavel DimitrovMartin J. TerrellKrishnan Kumaran
    • Matthias G. ImhofDominique G. GillardStefan HussenoederPavel DimitrovMartin J. TerrellKrishnan Kumaran
    • G01V1/00G06F17/00
    • G01V1/003G01V1/301G01V2210/64G06F17/00
    • Method for analysis of hydrocarbon potential of subterranean regions by generating surfaces or geobodies and analyzing them for hydrocarbon indications. Reflection-based surfaces may be automatically created in a topologically consistent manner where individual surfaces do not overlap themselves and sets of multiple surfaces are consistent with stratigraphic superposition principles. Initial surfaces are picked from the seismic data (41), then broken into smaller parts (“patches”) that are predominantly topologically consistent (42), whereupon neighboring patches are merged in a topologically consistent way (43) to form a set of surfaces that are extensive and consistent (“skeleton”). Surfaces or geobodies thus extracted may be automatically analyzed and rated (214) based on a selected measure (213) such as AVO classification or one or more other direct hydrocarbon indicators (“DHI”). Topological consistency for one or more surfaces may be defined as no self overlap plus local and global consistency among multiple surfaces (52).
    • 通过产生表面或地球体分析地下区域的碳氢化合物潜力并分析烃类适应性的方法。 基于反射的表面可以以拓扑一致的方式自动创建,其中各个表面不重叠,多个表面的集合与地层叠加原理一致。 从地震数据(41)拾取初始表面,然后将其分解成主要是拓扑一致的较小部分(“补丁”)(42),于是以拓扑一致的方式(43)合并相邻的补丁以形成一组表面 这是广泛和一致的(“骨架”)。 可以基于诸如AVO分类或一个或多个其他直接碳氢化合物指示器(“DHI”)的选定措施(213)自动分析和评估(214)所提取的表面或地球体。 一个或多个表面的拓扑一致性可以被定义为在多个表面之间没有自重叠加局部和全局一致性(52)。
    • 9. 发明授权
    • Detection of features in seismic images
    • 地震图像特征检测
    • US08363510B2
    • 2013-01-29
    • US12741133
    • 2008-10-31
    • Krishnan KumaranJingbo Wang
    • Krishnan KumaranJingbo Wang
    • G01V1/00
    • G01V1/288
    • A computer implemented method for the detection of features such as faults or channels in seismic images. First, edges are detected in a smoothed seismic image (106). To detect a fault line, an image intensity of the edges is projected in multiple spatial directions, for example by performing a Radon transform (118). The directions of maximum intensity are used to define a fault line (124c). To detect channels, smooth curves are identified within the detected edges (810). Sets of parallel smooth curves (812a) are then identified and used to define channels (812).
    • 一种用于检测地震图像中的故障或通道等特征的计算机实现方法。 首先,在平滑的地震图像中检测边缘(106)。 为了检测故障线,例如通过执行Radon变换(118),沿多个空间方向投影边缘的图像强度。 最大强度的方向用于定义断层线(124c)。 为了检测通道,在检测到的边缘内识别平滑曲线(810)。 然后识别并行平滑曲线组(812a)并用于定义通道(812)。