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Processing and interpretation of JERS-1 Synthetic Aperture Radar (SAR) image of Cepu and its surrounding areas, Central Java Province, Indonesia

机译:印度尼西亚中爪哇省宿务市及其周边地区JERS-1合成孔径雷达(SAR)图像的处理和解释

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摘要

[ABSTRACT] Geological as well as lithological interpretations of subsurface condition from Radar image are of great interest. Conventionally, geological features are derived visually from the images. Patterns associated with geological structures/ features are recognized. Attempts to interpret lithological as well as structural geological features deeper than 1 - 10 meters are of course challenging. This research is in the early stage of an attempt to derive lithological and geological features from Radar image conducted in the Department of Geophysical Engineering of Institute of Technology Bandung, Indonesia. In this stage, we tried to derive geological structures and other features visually from JERS-1 SAR data from Cepu area in Central Java Province, Indonesia, in which a huge oil reservoir located. Conventional image processing flows applied on the data could improve data quality that lead to more interpretability of the data. Eleven anticlinal folds and one faulted anticlinal fold were detectable. These folds could be identified based on their characteristics: coarse textures and high brightness values, folded form or horizontally folded and symmetrical or repetitive patterns. Shear fault structures could also be identified based on the appearance of lineaments intersecting folds. A small difference in structure orientation interpretation from image-derived structures and the geological structure map could be resulted from the error in the process for geometric correction, especially for structures located outside ASTER image coverage acting as geometrical correction reference. Even for structures inside the ASTER image coverage, Digital Elevation Modeling (DEM) technique should be incorporated in the processing for better results in the determination of structures orientation.
机译:[摘要]雷达图像对地下条件的地质学和岩性解释引起了人们的极大兴趣。传统上,地质特征是从图像上视觉获得的。识别与地质结构/特征有关的模式。试图解释比1-10米深的岩性和结构地质特征当然是具有挑战性的。这项研究是在印尼万隆技术学院地球物理工程系进行的从雷达图像推导岩性和地质特征的尝试的早期阶段。在此阶段,我们尝试从印度尼西亚中爪哇省Cepu地区的JERS-1 SAR数据中直观地导出地质结构和其他特征,该地区位于一个巨大的油藏中。应用于数据的常规图像处理流程可以提高数据质量,从而提高数据的可解释性。可检测到11条背斜褶皱和1条背斜褶皱。这些折痕可以根据其特征进行识别:粗糙的纹理和高亮度值,折痕或水平折叠以及对称或重复的图案。剪切断层的结构也可以根据与褶皱相交的细纹的出现来确定。与图像衍生结构和地质结构图的结构取向解释之间的微小差异可能是由于几何校正过程中的错误所致,特别是对于位于ASTER图像覆盖范围之外的用作几何校正参考的结构。即使对于ASTER图像覆盖范围内的结构,也应将数字高程建模(DEM)技术应用于处理过程中,以便在确定结构方向时获得更好的结果。

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