Detection of buried channels using color stack method (RGB)

pectral decomposition of time series has a significant role in seismic data processing nd interpretations. Since the earth acts as a low-pass filter, it changes the frequency ontent of the passing seismic waves. Conventional methods of representing signals in a ime domain and frequency domain cannot show the time information and the frequency nformation simultaneously. Time-frequency transforms an upgraded spectral ecomposition to a new step and can show time and frequency information imultaneously. ime-frequency transforms generate a high volume of spectral components, which ontain useful information about the reservoir and can be decomposed into single requency volumes. These single frequency volumes can overload the limited space of a omputer hard disk and are not easy for an interpreter to investigate them individually; herefore, it is important to use methods to decrease the volume without losing nformation. The frequency slices are thus separated from these volumes and used for an nterpretation. n this study, three different methods were used to represent a buried channel. In the irst method, the numbers of the single frequency slices were investigated, variations of he frequency amplitudes in the slices were observed, and an expert interpreter could btain some information about the channel content and lateral variation. Since different requencies contain different types of information (low frequencies are sensible to hannel content and high frequencies are sensible to channel boundaries), none of the lices were able to show all information simultaneously. In the next two methods using a olor stacking method, the RGB plots were constructed which, due to the different requency content, resulted in more information than the frequency slice representation method. An RGB image, sometimes referred to as a true color image, is an image that defines red, green, and blue color components for each individual pixel and has an intensity between 0 and 1. In this study, RGB plots were constructed in two different manners, RGB plots based on conventional RGB plot methods and RGB plots using basis functions. In the conventional method, three different frequency slices were mapped against the red, green and blue components. Although this method obviates some drawbacks of the single frequency plots, it uses only three slices and practically ignores a big part of information. Using basis functions and defining windows, the interpreter was able to introduce some frequency intervals and plot them against the primary components and use the total bandwidth or its major part. Three simple raised cosine functions having different frequency centers and different periods were chosen. The image quality strongly depended on these two parameters. Longer window widths will introduce longer frequency widths into every primary component and resulted in smoother color combinations for images and very short periods had the same results as the conventional RGB plot method. Different centers showed different details. Low frequency centers showed channel content properties, and high frequency centers showed channel boundaries and fine branches.In this study, the spectral decomposition was first performed on land seismic data from an oil field in Iran using a short time Fourier (STFT) transform and an S transform. Then three demonstration methods were applied for channel detection. Finally it was shown that how RGB color stacking method represented buried channels in more precise images and how a basis function based RGB represents better results than the conventional RGB method.