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    • 1. 发明授权
    • Method and apparatus for detecting and measuring elastic anisotropy
    • 用于检测和测量弹性各向异性的方法和装置
    • US4912979A
    • 1990-04-03
    • US310485
    • 1989-02-14
    • Carl H. SondergeldChandra S. RaiRichard M. Alford
    • Carl H. SondergeldChandra S. RaiRichard M. Alford
    • G01N29/07G01N33/24
    • G01N29/07G01N33/24
    • A novel method for detecting and measuring elastic anisotropy in a sample of the earth's formations is provided. A dyad of time series signal representative of the sample's response to imparted shear waves is recorded. The dyad of time series signals can then be processed to detect and measure elastic anisotropy in the sample. More particularly, the dyad of time series signals are collected by imparting shear waves having first and second polarizations into the samples with a shear wave transducer and recording the sample's response to each of the imparted shear waves by shear wave transducers having first and second polarizations. In one embodiment of the invention, the dyad of time series signals can be diagonalized to detect and measure elastic anisotropy in the sample. In another embodiment, the dyad of time series signals can be processed for a plurality of rotation angles and the resulting rotated dyad of time series signals can be displayed to detect and measure elastic anisotropy in the sample.
    • 提供了一种用于检测和测量地球样品中的弹性各向异性的新方法。 记录代表样品对赋予剪切波的响应的时间序列信号的二元组。 然后可以处理时间序列信号的二元组,以检测和测量样品中的弹性各向异性。 更具体地,通过用剪切波传感器将具有第一和第二极化的剪切波施加到样品中来收集时间序列信号的二元组,并通过具有第一和第二偏振的剪切波变换器记录样品对每个施加的剪切波的响应。 在本发明的一个实施例中,可以将时间序列信号的二元对角化以检测和测量样品中的弹性各向异性。 在另一个实施例中,可以处理多个旋转角度的时间序列信号的二元组,并且可以显示所产生的旋转的时间序列信号,以检测和测量样品中的弹性各向异性。
    • 2. 发明授权
    • Method an system of geophysical exploration
    • 方法探索地球物理系统
    • US4996421A
    • 1991-02-26
    • US264926
    • 1988-10-31
    • Chandra S. RaiCarl H. Sondergeld
    • Chandra S. RaiCarl H. Sondergeld
    • G01N21/31G01N21/35G01N33/24
    • G01N21/3563G01N33/241G01N2021/3196G01N2021/3572G01N2021/3595
    • A system and method of geophysical exploration is described whereby composition logs of the minerals comprising the formations surrounding a wellbore can be obtained. Samples of the formations surrounding a wellbore are obtained at selected intervals along the length of the wellbore. Each of the core samples is irradiated with electromagnetic radiation and a spectral response signal, representative of the electromagnetic response of each sample to the electromagnetic radiation is recorded. Peaks in the spectral response signals are located and correlated with minerals exhibiting similar electromagnetic characteristic response peaks. Since the samples were obtained from known depths within the wellbore, a composition log of the minerals comprising the formations surrounding the wellbore can be prepared displaying the minerals identified as a function of depth in the wellbore.
    • 描述了地球物理勘探的系统和方法,其中可以获得包含围绕井眼的地层的矿物的组成原木。 沿着井筒的长度以选定的间隔获得围绕井筒的地层的样品。 每个核心样品用电磁辐射照射,并且记录表示每个样品对电磁辐射的电磁响应的光谱响应信号。 光谱响应信号中的峰位于表现出类似电磁特征响应峰的矿物并与其相关。 由于样品是从井筒内的已知深度获得的,所以可以制备包含井筒周围的地层的矿物的组成成分,显示在井眼中被鉴定为深度函数的矿物质。
    • 9. 发明授权
    • Method for determining in-situ formation properties
    • 确定原位形成性质的方法
    • US4831530A
    • 1989-05-16
    • US67671
    • 1987-06-26
    • Chandra S. Rai
    • Chandra S. Rai
    • G01V1/30
    • G01V1/30
    • A method for determining in-situ formation properties is provided. Through regression analyses, empirical systematic relations are obtained using measures of formation properties obtained form formation samples of at lest one reference well over a range of effective pressures and pore fluids. The formation properties are selected from the group comprising shear velocity, compressional velocity, as well as porosity and mineralogy content. Direct measurements of at least two in-situ formation properties selected from the group of shear velocity, compressional velocity, porosity and mineralogy content are obtained for an exploratory well. The empirical systematic relations of formation properties are inverted to determine estimates of the balance of the insitu formation properties selected from the group including shear wave velocity, compressional wave velocity, porosity and mineralogy content not directly measured.
    • 提供了一种确定原位形成特性的方法。 通过回归分析,通过在有效压力和孔隙流体范围内至少一个参考井的形成样品获得的地层性质的测量获得经验系统关系。 形成性质选自剪切速度,压缩速度以及孔隙率和矿物学含量。 对于探索井,获得从剪切速度,压缩速度,孔隙度和矿物学含量组中选择的至少两个原位形成性质的直接测量。 反演地层性质的经验系统关系,以确定从直接测量的剪切波速度,压缩波速度,孔隙度和矿物含量组中选出的地层形成性质的平衡估计。
    • 10. 发明授权
    • Method for estimating formation lithology
    • 估计地层岩性的方法
    • US4907206A
    • 1990-03-06
    • US226354
    • 1988-07-29
    • Chandra S. RaiKenneth E. Hanson
    • Chandra S. RaiKenneth E. Hanson
    • G01V1/50
    • G01V1/50
    • A novel method of geophysical exploration is described for obtaining estimates the formation lithology from measures of formation anisotropy. First and second measures of formation anisotropy can be transformed into estimates of formation lithology by crossplotting them onto a lithology diagram. In one embodiment of the present invention, the lithology diagram comprises two separate axes representing measures of formation azimuthal anisotropy and transverse isotropy for a selected formation property which defines regions of separate lithologies. The lithology diagram can provide a novel means for discriminating formation lithology from the measures of formation anisotropy.
    • 描述了一种新的地球物理勘探方法,用于从地层各向异性测量中获得地层岩性的估计。 地层各向异性的第一和第二措施可以通过将它们交叉绘制到岩性图上而转化为地层岩性的估计。 在本发明的一个实施例中,岩性图包括两个独立的轴,其表示对限定分开的岩性区域的选定地层特性的形成方位各向异性和横向各向同性的测量。 岩性图可以提供一种用于区分地层岩性与地层各向异性测量的新手段。