光谱分解和RGB混合在Asri盆地“S”水道圈定中的应用

S. A. Piranti, S. Zulivandama, N. C. Aryanto, A. Nur, I. Syafri
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引用次数: 0

摘要

Gita段是位于南苏门答腊岛东部Asri盆地的Talang Akar组的一部分,该组被称为油气储层。该组由辫状河道、曲流河道、河流三角洲、河口等沉积体系组成。河道系统是Asri盆地发育的一个有趣的系统,然而,由于河道的厚度导致其外观通常接近或低于地震分辨率,因此获得Asri盆地的河道分布具有相当大的挑战性,并且目标下方的煤的存在也影响了“S”砂在地震数据中的印象。在这项研究中,光谱分解和RGB混合已经成功地识别了“S”砂。RGB混合图以15 Hz为低频,45 Hz为中频,75 Hz为高频提取。在RGB混合图上进行解释,发现“S”砂属曲流河道沉积体系,河道主要走向为东北-西南。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Application of Spectral Decomposition and RGB Blending for Delineation of “S” Channel At Asri Basin
Gita member is part of Talang Akar Formation is known as hydrocarbon reservoir at Asri Basin, eastern part of South Sumatra. This formation consists of several depositional systems such as braided channel, meandering channel, fluvial-deltaic, and estuarine system. A channel system was an interesting system developed in the Asri Basin, however, to get the channel distribution in Asri Basin is quite challenging because the thickness of the channels caused its appearance is generally close or under seismic resolution, the existence of coal below our target also affects the impression of “S” sand on seismic data. In this study, spectral decomposition and RGB Blending have been successful to identify “S” sand. RGB Blending map is extracted from 15 Hz as low frequency, 45 Hz as middle frequency, and 75 Hz as high frequency. Our interpretation was applied at RGB Blending map and reveal the “S” sand is classified as a meandering channel depositional system with the main direction of the channel is Northeast – Southwest. 
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