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New Image Process Technique Reveals New Hidden Formation Structures Using Anisotropy and Dip Images

机译:新的图像过程技术使用各向异性和DIP图像揭示了新的隐藏形成结构

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A new image processing technique has been developed in which resistivity-based image data is used to create new images based on anisotropy. The advantage of imaging tools is that they can provide high resolution geological information in 3 dimensions (i.e., vertically and azimuthally around the borehole). Therefore, it is possible to interpret this data in more detail than with logs that produce only depth-associated information. Consider a resistivity imager that takes an array of measurements around the borehole. This information is composed of an array of measurements much like the pixels in a photograph. These pixels can be displayed so that the position of the points is aligned with depth in the vertical axis and angular displacement in the horizontal axis in a frame of data. Based on the spatial orientation of the data, it is possible to upscale these points to determine the up-scaled horizontal (Rh) and vertical resistivity (Rv) associated with these points. The entire frame of data is resolved into a single-valued point with anisotropy. By repositioning the center point of the frame, a new anisotropy is then determined and an image log is created by processing the entire image. This upscale anisotropy image assumes that the anisotropy is relative to the borehole. In another step, the axis of the data frame is rotated until a minimum anisotropy is determined, resulting in anisotropy and a dip value associated with that point. As a result, both an anisotropy and dip image can be created by processing the entire image in this manner. These new anisotropy and dip angle images open up an entirely new way of analyzing image data and reveal hidden structures that are not readily apparent in the original image. This new image processing method is used to analyze resistivity image logs, and the results show dramatic new images that enhance the understanding of the geologic structures. .
机译:已经开发了一种新的图像处理技术,其中基于电阻率的图像数据用于基于各向异性创建新图像。成像工具的优点是它们可以在3尺寸(即,围绕钻孔周围)提供高分辨率的地质信息。因此,可以比产生仅生成深度相关信息的日志更详细地解释该数据。考虑一种电阻率成像仪,其在钻孔周围采用一系列测量。该信息由一系列测量组成,就像照片中的像素一样。可以显示这些像素,使得点的位置与垂直轴的深度对准,并且在数据帧中的水平轴中的角位移。基于数据的空间方向,可以高档这些点以确定与这些点相关联的上缩放的水平(RH)和垂直电阻率(RV)。整个数据帧被解析为具有各向异性的单值点。通过重新定位帧的中心点,然后确定新的各向异性,并且通过处理整个图像来创建图像日志。该高档各向异性图像假定各向异性相对于钻孔。在另一步骤中,数据帧的轴旋转,直到确定最小各向异性,导致各向异性和与该点相关联的倾角值。结果,可以通过以这种方式处理整个图像来创建各向异性和DIP图像。这些新的各向异性和倾角图像开辟了一种分析图像数据的全新方法,并揭示了原始图像中不容易明显的隐藏结构。这种新的图像处理方法用于分析电阻率图像日志,结果显示了增强对地质结构的理解的戏剧性新图像。 。

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