SYSTEM AND METHOD FOR VELOCITY ANOMALY ANALYSIS
    91.
    发明公开
    SYSTEM AND METHOD FOR VELOCITY ANOMALY ANALYSIS 审中-公开
    系统和方法的速度异常分析

    公开(公告)号:EP2926172A1

    公开(公告)日:2015-10-07

    申请号:EP13767223.4

    申请日:2013-09-17

    IPC分类号: G01V1/30

    摘要: Methods of analyzing velocity models include defining velocity anomaly models for a subsurface region under study. The velocity anomaly model is overlain on a seismic stack image to produce a hybrid velocity/amplitude model. Regions in which stack amplitudes are coincident with velocity anomalies may be interpreted as representing structures of interest. In an embodiment, clathrate deposits are identified using the hybrid model. In an embodiment, geobodies are identified, and velocity anomalies are constrained by the geobodies.

    摘要翻译: 分析速度模型的方法包括为研究中的地下区域定义速度异常模型。 速度异常模型覆盖在地震叠加图像上以产生混合速度/振幅模型。 堆振幅与速度异常一致的区域可以被解释为表示感兴趣的结构。 在一个实施例中,使用混合模型来识别包合物沉积物。 在一个实施例中,地质体被识别,并且速度异常被地质体限制。

    ANALYZING SEISMIC DATA
    93.
    发明公开
    ANALYZING SEISMIC DATA 审中-公开
    地震数据分析

    公开(公告)号:EP2914984A1

    公开(公告)日:2015-09-09

    申请号:EP13852001.0

    申请日:2013-08-30

    IPC分类号: G01V1/28

    摘要: A system and methods for analyzing seismic data are provided herein. The method includes identifying, via a computing device, a representation of a seismic data set (1802) and determining a number of feature descriptors corresponding to each of a number of aggregates within the representation (1804). The method also includes identifying a query relating to the representation and one or more vocabulary definitions relating to the query (1806), analyzing the representation to compute a likelihood that each of the aggregates satisfies the query (1808), and returning a result of the query (1810).

    METHOD AND SYSTEM FOR CHECKPOINTING DURING SIMULATIONS
    95.
    发明公开
    METHOD AND SYSTEM FOR CHECKPOINTING DURING SIMULATIONS 审中-公开
    CHECKPOINTING工艺和系统在使用过程中模拟

    公开(公告)号:EP2572292A1

    公开(公告)日:2013-03-27

    申请号:EP11783895.3

    申请日:2011-03-14

    IPC分类号: G06F15/173

    摘要: Method and system for more efficient checkpointing strategy in cross correlating (316) a forward (328) and backward (308) propagated wave such as in migrating (326) or inverting seismic data. The checkpointing strategy includes storing in memory forward simulation data at a checkpointed time step, wherein the stored data are sufficient to do a cross correlation at that time step but not to restart the forward simulation. At other checkpoints, a greater amount of data sufficient to restart the simulation may be stored in memory (314). Methods are disclosed for finding an optimal combination, i.e. one that minimizes computation time (1132), of the two types of checkpoints for a given amount of computer memory (1004), and for locating a checkpoint at an optimal time step (306, 1214, 1310). The optimal checkpointing strategy (1002) also may optimize (1408) on use of fast (1402) vs. slow (1404) storage.

    Determining a Position of a Geological Layer Relative to a Wavelet Response in Seismic Data
    97.
    发明公开
    Determining a Position of a Geological Layer Relative to a Wavelet Response in Seismic Data 审中-公开
    确定地质相对的层的位置,以在地震数据小波响应

    公开(公告)号:EP2420863A2

    公开(公告)日:2012-02-22

    申请号:EP11177448.5

    申请日:2011-08-12

    发明人: Peirle, Thomas

    IPC分类号: G01V1/30

    摘要: Determining geological layer location in a subterranean formation, including receiving seismic data representing an interaction of the geological layer with propagation of a seismic wave, identifying a source wavelet representing a portion of the seismic wave impinging on a boundary of the geological layer, providing a geological layer template of the geological layer including primary and secondary reflection interfaces associated with reflectivity based on material properties of the geological layer, generating a wavelet response template by applying the source wavelet to the geological layer template using a mathematical convolution operation to model seismic wave interference caused by the primary and secondary reflection interfaces, identifying an extremum of the seismic data, and determining, based on the extremum, the location of the geological layer in the subterranean formation using the wavelet response template.

    摘要翻译: 在地下地层中确定的地质层的位置,包括:接收在与地震波传播的地质层的交互表示的地震数据,识别表示地震波入射到地质层的边界上的一部分上的震源子波,提供了地质 包括与基于所述地质层的材料性能的反射率相关联的初级和次级反射界面,通过使用数学卷积手术模型地震波干扰引起的施加源小波地质层模板生成小波响应模板地质层的层模板 通过初级和次级反射界面,识别地震数据的极值,并且确定性开采,基于极值,利用小波响应模板在地下地层地质层的位置。

    Determining connectivity architecture in 2-D and 3-D heterogeneous data
    99.
    发明公开
    Determining connectivity architecture in 2-D and 3-D heterogeneous data 审中-公开
    在异源2D和3D数据中的Bestimmung der Verbindungsarchitektur

    公开(公告)号:EP2098887A1

    公开(公告)日:2009-09-09

    申请号:EP08003927.4

    申请日:2008-03-03

    IPC分类号: G01V1/00

    摘要: A method is disclosed for determining the connectivity architecture of a hydrocarbon reservoir in terms of locally optimal paths between selected source points, e.g. wells. In one embodiment of the invention, a fast-marching method (133) is used to compute the distance field (or the time of arrival field) from N selected source points in a heterogeneous media, i.e. in a non-uniform velocity field. This is done by propagating N labeled (132) fronts simultaneously from N objects. Then, a method (134) is disclosed for detecting Voronoi curves or Voronoi surfaces, where fronts of differing labels meet each ether. Then, saddle points are found on the Voronoi curves or surfaces (135), and each saddle point is used to determine a locally optimal path (136) between a pair of equidistant (from the saddle point), closest (to the saddle point) source points.

    摘要翻译: 公开了一种用于根据所选源点之间的局部最佳路径来确定烃储层的连通性结构的方法,例如, 井。 在本发明的一个实施例中,快速行进方法(133)用于从非均匀介质中的N个选择的源点,即在非均匀速度场中计算距离场(或到达时间场)。 这通过从N个对象同时传播N个标记的(132)前端来完成。 然后,公开了一种用于检测Voronoi曲线或Voronoi曲面的方法(134),其中不同标签的前端满足每个醚。 然后,在Voronoi曲线或表面(135)上找到鞍点,并且每个鞍点用于确定最接近(相对于鞍座点)的一对等距(从鞍点)的局部最佳路径(136) 来源点。