使用接缝雕刻调整地震数据大小

Julián L. Gómez, D. Velis
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摘要

通过减小地震图像的尺寸,可以加快地震资料的解释速度。裁剪、抽取和调整大小(平均后抽取)是实现这些目标的一些众所周知的技术。seam carving (SC)不是定期地从输入图像中删除某些行和列(抽取)或预定义的行和列组(裁剪),而是在保留输入图像内容的同时丢弃输入图像中信息量最少的区域。SC是一种计算机视觉算法,最初设计用于调整自然图像的大小,据我们所知,以前没有应用于调整地球物理数据的大小。我们建议采用SC来提供更小,但具有代表性的地震图像,这些图像包含原始数据中最相关的结构和纹理,并具有振幅保存。这些简化后的图像可以被地震解释人员用来处理日常的行业需求和截止日期,因为他们可以用更少的计算资源和更短的时间框架来分析过滤器和地震属性的结果。本质上,SC依赖于能量算子和动态优化来从输入图像迭代地寻找最佳像素轨迹,直到获得所需的图像尺寸。我们通过使用基于著名的Sobel幅度的能量算子来修改原始SC算法,该算子在两个维度上都具有较高的还原率和最小的伪影。我们通过一个玩具例子和月球表面的图像来说明SC。然后,将该方法应用于由两个地震剖面和一个地震振幅时间片组成的现场地震数据的大小调整。结果表明,与抽取或传统的调整大小相反,SC提供了有意义的简化地震图像,保留了原始数据的主要特征。
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Seismic Data Resizing Using Seam Carving
Seismic data interpretation can be accelerated by reducing the size of the seismic images. Cropping, decimation, and resizing (decimation after averaging), are some well-known techniques to accomplish these goals. Rather than regularly removing certain rows and columns (decimation), or predefined groups of rows and columns (cropping) from the input image, seam carving (SC) discards the least informative regions of the input image while preserving its content. SC is a computer vision algorithm originally devised to resize natural images that, to our best knowledge, had not been applied to resize geophysical data previously. We propose to adopt SC to deliver smaller, yet representative, seismic images that contain the most relevant structures and textures of the original data with amplitude preservation. These reduced images can be used by seismic interpreters to cope with day-to-day Industry demands and deadlines since they can analyze the results of filters and seismic attributes with less computational resources and in shorter time frames. Essentially, SC relies on an energy operator and dynamic optimization to find the optimal pixel trajectories to carve from the input image iteratively until the desired image size is attained. We modify the original SC algorithm by using an energy operator based on the well-known Sobel magnitude that grants high reduction rates in both dimensions with minimum artifacts. We illustrate SC by means of a toy example and an image from the Moon’s surface. Then, the proposed method is applied to resize field seismic data that comprise two seismic sections and one seismic amplitude time-slice. The results demonstrate that SC, contrarily to decimation or conventional resizing, provides meaningful reduced seismic images that preserve the main features of the original data.
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