Geological Prediction Technology
    6.
    发明申请
    Geological Prediction Technology 审中-公开
    地质预测技术

    公开(公告)号:US20160146973A1

    公开(公告)日:2016-05-26

    申请号:US14950906

    申请日:2015-11-24

    Inventor: Luke Johnson

    CPC classification number: G01V99/005 G01V1/306 G01V2210/665

    Abstract: A method of processing geological data is provided for input to a geostatistical modelling algorithm to predict a value for a parameter relating to a physical property of the Earth. An input data set corresponding to a measured geological parameter is processed to determine a characteristic function of the input data with respect to a geological measure. The input data is transformed to reduce spatial bias with respect to the geological distance measure by applying an inverse function. A statistical weighting is calculated for the transformation and the transformation and weighting are used to predict a representative value of the physical property corresponding to the measured geological parameter. A data processing apparatus and computer program product are also provided.

    Abstract translation: 提供了一种处理地质数据的方法,用于输入到地统计建模算法,以预测与地球的物理属性有关的参数的值。 对与测量的地质参数相对应的输入数据集进行处理,以确定相对于地质测量的输入数据的特征函数。 通过应用反函数来转换输入数据以减少相对于地质距离测量的空间偏差。 计算转换的统计加权,使用变换和加权来预测与测量的地质参数对应的物理性质的代表值。 还提供了数据处理装置和计算机程序产品。

    ESTIMATING INTERVAL VELOCITIES
    7.
    发明申请
    ESTIMATING INTERVAL VELOCITIES 审中-公开
    估算间隔时间

    公开(公告)号:US20160091621A1

    公开(公告)日:2016-03-31

    申请号:US14962905

    申请日:2015-12-08

    Inventor: Arild BULAND

    CPC classification number: G01V1/303 G01V2210/6222 G01V2210/665 G01V2210/667

    Abstract: A method of estimating a velocity of a geological layer includes a. providing a first, initial model including an interval velocity associated with a subsurface location and an uncertainty associated with the interval velocity; b. providing data including an actual or approximated root-mean-square (RMS) velocity associated with a subsurface location and an uncertainty associated with the RMS velocity; and c. estimating a second model including an interval velocity associated with a subsurface location and an uncertainty associated with the interval velocity, based on the interval velocity and the uncertainty of the first model, and the RMS velocity and the uncertainty of the data.

    Abstract translation: 估计地质层速度的方法包括:a。 提供包括与地下位置相关联的间隔速度和与间隔速度相关联的不确定性的第一初始模型; b。 提供包括与地下位置相关联的实际或近似均方根(RMS)速度和与RMS速度相关联的不确定性的数据; 和c。 基于间隔速度和第一模型的不确定性以及RMS速度和数据的不确定性来估计包括与地下位置相关联的间隔速度和与间隔速度相关联的不确定性的第二模型。

    System and method for lacunarity analysis
    8.
    发明授权
    System and method for lacunarity analysis 有权
    用于空洞分析的系统和方法

    公开(公告)号:US09285502B2

    公开(公告)日:2016-03-15

    申请号:US12633630

    申请日:2009-12-08

    CPC classification number: G01V11/00 G01V2210/665

    Abstract: A system for and computer implemented method for analysis of data representative of subsurface properties of a subsurface region. The method includes transforming the data representative of subsurface properties of the subsurface region into transformed data in accordance with a selected criterion. A three dimensional window geometry to be applied to the transformed data is selected, based, at least in part, on expected feature sizes present, data sampling density and a size of the subsurface region. A plurality of values for a three dimensional lacunarity statistic are calculated by applying the selected three dimensional window geometry to randomly selected regions of the subsurface region, and correlating the calculated values to the subsurface properties of the subsurface region.

    Abstract translation: 一种用于分析代表地下地区地下特性的数据的计算机实现方法。 该方法包括根据所选择的标准将代表地下区域的地下特性的数据变换为变换数据。 至少部分地基于存在的预期特征尺寸,数据采样密度和地下区域的尺寸来选择要应用于变换数据的三维窗口几何形状。 通过将所选择的三维窗口几何应用于地下区域的随机选择的区域来计算三维空隙统计量的多个值,并将计算的值与地下区域的地下特性相关联。

    FREQUENCY-DOMAIN AUGMENTED TIME-DOMAIN FULL WAVEFIELD INVERSION
    9.
    发明申请
    FREQUENCY-DOMAIN AUGMENTED TIME-DOMAIN FULL WAVEFIELD INVERSION 审中-公开
    频域支持时域全波形反演

    公开(公告)号:US20150293246A1

    公开(公告)日:2015-10-15

    申请号:US14656389

    申请日:2015-03-12

    Abstract: A basically time-domain method for performing full wavefield inversion of seismic data to infer a subsurface physical property model (61), where however at least one quantity required for the inversion, such as the Hessian of the cost function, is computed in the frequency domain (64). The frequency-domain quantity or quantities may be obtained at only a few discrete frequencies (62), preferably low frequencies, and may be computed on a coarse spatial grid, thus saving computing time with minimal loss in accuracy. For example, the simulations of predicted data and the broadband gradient of the objective function may be computed in the time domain (67), and the Hessian matrix, approximated by its diagonal, may be computed in the frequency domain. It may be preferable to use time-domain and the frequency-domain solvers that employ different numerical schemes, such as finite-difference method, one-way wave equation, finite-element method (63).

    Abstract translation: 用于执行地震数据的全波场反演以推断地下物理属性模型(61)的基本时域方法(61),然而,在频率中计算反演所需的至少一个数量,例如成本函数的Hessian 域(64)。 可以仅在几个离散频率(62),优选低频率处获得频域量或量,并且可以在粗略的空间网格上计算,从而以最小的精度损失节省计算时间。 例如,可以在时域(67)中计算目标函数的预测数据和宽带梯度的模拟,并且可以在频域中计算由其对角线近似的Hessian矩阵。 使用有限差分法,单向波动方程,有限元法(63),采用不同数值方案的时域优化和频域求解器。

    METHOD OF CONSTRUCTING A GRID REPRESENTATIVE OF A PROPERTY DISTRIBUTION BY CONDITIONAL MULTIPOINT STATISTICAL SIMULATION
    10.
    发明申请
    METHOD OF CONSTRUCTING A GRID REPRESENTATIVE OF A PROPERTY DISTRIBUTION BY CONDITIONAL MULTIPOINT STATISTICAL SIMULATION 有权
    通过条件多点统计模拟构建财产分配网格代表的方法

    公开(公告)号:US20150131866A1

    公开(公告)日:2015-05-14

    申请号:US14538931

    申请日:2014-11-12

    Abstract: The invention is a method using a computer to construct a grid representative of the distribution of a physical property of an underground formation having application to petroleum reservoir development. A set of initial grid cells MI containing at least one conditioning point PC is defined. Each cell MI is then visited and assigned a value representative of the property using a filling method. At least one unvisited cell (MNV1, MNV2) adjacent to at least one already visited cell MV is then identified, and the number N of adjacent cells MV is determined for each cell (MNV1, MNV2). Each cell (MNV1, MNV2) is then visited and filled according to the decreasing values of N. The stages of identification and filling of cells (MNV1, MNV2) are repeated until each cell of the grid has been visited.

    Abstract translation: 本发明是一种使用计算机构建代表应用于石油储层开发的地下地层的物理性质分布的方法的方法。 定义了一组包含至少一个调节点PC的初始网格单元MI。 然后使用填充方法访问每个细胞MI并分配代表该性质的值。 然后识别与至少一个已经访问的单元MV相邻的至少一个未访问单元(MNV1,MNV2),并且为每个单元(MNV1,MNV2)确定相邻单元MV的数量N. 然后根据N的减小值访问并填充每个小区(MNV1,MNV2)。重复确认和填充小区(MNV1,MNV2)的阶段,直到网格的每个小区被访问为止。

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