应用探地雷达法研究Panasogan-Waturanda地层接触边界区层状结构

E. Ibrahim, W. Parnadi
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引用次数: 0

摘要

研究了在爪哇中部Kebumen Karangsambung的Panosogan组和Waturanda组之间的接触区域进行的共偏移剖面测量的探地雷达(GPR)数据。采用探地雷达RAMAC系统。该研究的目的是识别和消除表面散射噪声和衰减效应,对地下分层结构进行成像,并确定Panosogan组和Waturanda组之间的接触区域。处理后的数据通过瞬时属性和所谓的联合时频(JTFA)分析进行分析。研究结果表明,雷达图中出现的一些衍射图样是由表面物体的散射引起的。这些可以通过f-k过滤和迁移来消除。地下电学特性与天线电学特性阻抗不匹配导致的衰荡效应难以消除。但是,在JTF表示中可以很好地识别和分析它。瞬时属性和JTF分析被证明是成像接触区域和亚表面层状结构的有用工具。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Study of Layered Structure on Contact Boundary Area of Formation Panasogan-Waturanda by Applying Ground Penetrating Radar Method
Study on Ground-penetrating radar (GPR) data from a common-offset profiling measurement carried out in the contact area between Panosogan and Waturanda Formations in Karangsambung, Kebumen – Central of Java is done. GPR RAMAC system is utilized. The aim of the study is to recognize and eliminate surface-scattering noise and ring-down effects, to image subsurface layered structure and to identify a contact area between Panosogan and Waturanda Formations. The processed data were analyzed with the help of instantaneous attributes and the so-called joint time frequency (JTFA) analysis. Study results show that some diffraction patterns appeared in radargram are resulting from scattering of surface-objects. These can be eliminated with f-k filtering and migration. Ring-down effect resulted from impedance mismatch between subsurface electrical properties and those of antenna is difficult to eliminate. However, it can be well recognized and analyzed in the JTF representation. Instantaneous attributes and JTF analysis are proved to be useful tools in imaging the contact area and subsurface layered structures.
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