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    • 11. 发明授权
    • Determining formation parameters using electromagnetic coupling components
    • 使用电磁耦合元件确定地层参数
    • US08841913B2
    • 2014-09-23
    • US13412942
    • 2012-03-06
    • Jian YangQiming LiJean Seydoux
    • Jian YangQiming LiJean Seydoux
    • G01V3/10G01V3/28
    • G01V3/28
    • A method and a downhole tool determine one or more parameters of a formation traversed by a borehole where at least a portion of the formation has substantially parallel boundaries. A tool is disposed in the borehole that includes a transmitter having a dipole moment at an angle θT with respect to a longitudinal axis of the tool, a receiver having a dipole moment at an angle θR with respect to the longitudinal axis of the tool and a rotational position indicator. The transmitter-receiver pair transmits an electromagnetic signal while rotating the tool, receives the electromagnetic signal to produce a measured signal, and determine(s) the formation parameters for the portion of the formation having substantially parallel boundaries based on the measured signal.
    • 方法和井下工具确定由钻孔穿过的地层的一个或多个参数,其中地层的至少一部分具有基本上平行的边界。 一种工具设置在钻孔中,该工具包括具有角度角度的偶极矩的发射器;相对于工具的纵向轴线的T;具有角度角度的偶极矩的接收器;相对于 工具和旋转位置指示器。 发射机 - 接收机对在旋转工具的同时传输电磁信号,接收电磁信号以产生测量信号,并且基于测量的信号确定具有基本上平行边界的地层部分的地层参数。
    • 14. 发明授权
    • Multilevel workflow method to extract resistivity anisotropy data from 3D induction measurements
    • 从三维感应测量中提取电阻率各向异性数据的多级工作流程方法
    • US08433518B2
    • 2013-04-30
    • US12888232
    • 2010-09-22
    • Dzevat OmeragicKeli SunQiming LiTarek Habashy
    • Dzevat OmeragicKeli SunQiming LiTarek Habashy
    • G01V1/40G01V3/10G06G7/48
    • G01V3/20G01V3/28
    • A method is provided for determining formation resistivity, anisotropy and dip from wellbore measurements includes moving a well logging instrument through subsurface formations. The instrument includes longitudinal magnetic dipoles and at least one of tilted and transverse magnetic dipoles. Formation layer boundaries and horizontal resistivities of the formation layers are determined from longitudinal magnetic dipole measurements. Vertical resistivities of the formation layers are determined by inversion of anisotropy sensitive measurements. Improved vertical resistivities of the formation layers and dips are determined by inverting symmetrized and anti-symmetrized measurements. Improved vertical resistivities, improved boundaries and improved dips are determined by inversion of the all dipole measurements. Improved horizontal resistivities, further improved layer boundaries and further improved dips are determined by inversion of all dipole measurements.
    • 提供了一种用于确定井眼测量的地层电阻率,各向异性和倾角的方法,包括通过地下地层移动测井仪器。 仪器包括纵向磁偶极子和倾斜和横向磁偶极子中的至少一个。 由纵向磁偶极子测量确定地层的形成层边界和水平电阻率。 通过各向异性敏感测量的反演确定形成层的垂直电阻率。 通过反转对称和反对称测量来确定形成层和浸渍层的垂直电阻率的改善。 通过所有偶极子测量的反演来确定改善的垂直电阻率,改善的边界和改善的倾角。 通过所有偶极子测量的反演来确定改进的水平电阻率,进一步改善的层边界和进一步改善的下降。
    • 15. 发明授权
    • Triaxial antenna electromagnetic measurements
    • 三轴天线电磁测量
    • US08417455B2
    • 2013-04-09
    • US12975664
    • 2010-12-22
    • Lili ZhongQiming Li
    • Lili ZhongQiming Li
    • G01V1/40G01V3/00
    • E21B47/102G01V3/28
    • The present disclosure relates to a method to determine a formation property of a subsurface formation. A downhole logging tool having two or more antennas, at least one of the antennas being a non-co-located triaxial antenna, is provided. Azimuthally sensitive measurements are obtained using the antennas of the downhole logging tool. The measurements are fitted to a Fourier series having Fourier coefficients and the non-co-location of the triaxial antenna is compensated for by adjusting the Fourier coefficients. Compensated measurements are determined using the adjusted Fourier coefficients and the formation property of the subsurface formation is determined using the compensated measurements. The compensating may use one or more scale factors that depend on an amplitude, phase, and/or frequency of the received signal, and an alignment angle between the triaxial antenna and another of the antennas of the logging tool.
    • 本公开涉及确定地下地层的地层特性的方法。 提供具有两个或更多个天线的井下测井工具,所述天线中的至少一个是非共同定位的三轴天线。 使用井下测井工具的天线获得方位敏感测量。 将测量值拟合到具有傅立叶系数的傅立叶级数,并且通过调整傅里叶系数来补偿三轴天线的非共位置。 使用调整的傅里叶系数确定补偿测量,并使用补偿测量确定地下地层的形成特性。 补偿可以使用取决于接收信号的幅度,相位和/或频率以及三轴天线与测井工具的另一天线之间的对准角度的一个或多个比例因子。
    • 20. 发明申请
    • [METHODS AND SYSTEMS FOR RESISTIVITY ANISOTROPY FORMATION ANALYSIS]
    • [电阻率成像分析方法与系统]
    • US20050114030A1
    • 2005-05-26
    • US10604492
    • 2003-07-25
    • Cheng LiuQiming LiFrank ShrayJacques Tabanou
    • Cheng LiuQiming LiFrank ShrayJacques Tabanou
    • G01V3/20G06F19/00
    • G01V3/20
    • Techniques for determining a formation property by simplifying various two-geological-layer or multi-geological-layer models into a multi-electrical-layer model. A volume fraction of a layer in a multi-electrical-layer model is determined for an anisotropic region (sliding window) of the formation. The multi-electrical-layer electrical model includes a relative-lower-resistivity layer and a relative-higher-resistivity layer. A high-resolution resistivity measurement is used in the determination and resistivities for the relative-lower-resistivity layer and for the relative-higher-resistivity layer based on the volume fraction and bulk resistivity measurements of the anisotropic region are determined. The formation property is based on the volume fraction, the resistivity of the relative-lower-resistivity layer, the resistivity of the relative-higher-resistivity layer, a total porosity of the anisotropic region, and bulk resistivity measurements of the region.
    • 通过将各种地质层或多地质层模型简化为多电层模型来确定地层特性的技术。 针对地层的各向异性区域(滑动窗口)确定多电层模型中的层的体积分数。 多电层电气模型包括相对低电阻率层和相对较高电阻率的层。 在相对低电阻率层的测定和电阻率中使用高分辨率电阻率测量,并且基于各向异性区域的体积分数和体电阻率测量确定相对较高电阻率层。 形成性质基于体积分数,相对低电阻率层的电阻率,相对高电阻率层的电阻率,各向异性区域的总孔隙率和该区域的体电阻率测量值。