应用探地雷达探测印度中安达曼Baratang岛因构造作用而形成的洞室方位

N. Ramanujam, P. Prasad, A. Vignesh, S. Murti, Q. A. Rasool, K. B. Swapan, C. Ojha, A. J. Boopalan, P. Yuvaraj
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引用次数: 1

摘要

探地雷达(GPR)是探测小型(<;直径10m)的溶洞和裂隙。在中安达曼岛Baratang凸起的碳酸盐岩中,在1平方公里范围内发现了170个洞穴。由于印度板块与缅甸板块在安达曼西北部的斜向俯冲,形成了NE- SW和NW- SE走向的缝合。研究目的是利用探地雷达技术对碳酸盐岩断层模式进行定向验证。为了进行探地雷达调查,选择了两个相距400米的洞穴遗址。GPR - SIR-3000仪器采用双基地偶极天线布置,反射模式为驻点模式。利用40 MHz天线的样条数据计算的4个深度(时间)切片,在500 ns范围内反射穿过1号洞,长度为19 m,显示出明亮的线性特征,强烈的斑点位于3 m和11 m至18 m以下,竖井连接的不连续面在所有图中都追踪到25 m深度。利用40mhz 400 ns天线,在间隔4.0 m至总距离28 m的5个深度切片上,在2号洞的8.5 ~ 12.5 m深度处反射出明亮区域,扫描深度达到20 m。利用时间窗为250 ns的80 MHz天线,在2号洞的7个深度切片上反射到12.5 m深度,在8.5 ~ 12.5 m深度范围内显示出高分辨率的明亮区域。随着时间范围的减小,天线频率的增加,2号洞的空腔、裂缝和深度减小的反射分辨率比1号洞高。碳酸盐岩中由于先前的构造反射作用而诱发的裂缝和裂隙随后通过雨水的渗透和溶蚀而增大了裂缝和裂隙的尺寸。两处洞室方位各断面探地雷达深度(时间)切片均证实洞室延续方向为NW-SE方向和NE-SW方向。
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 Ground Penetrating Radar to detect orientation of cavities and caverns developed due to tectonic implication in Baratang Island, Middle Andaman, India
Ground Penetrating Radar (GPR) is an effective tool to detect small (<; 10m diameter) caves and fissures in karst terrain. 170 caves have been identified within 1 km2 area in uplifted carbonate rocks in Baratang Island of Middle Andaman. Due to oblique subduction of Indian plate with Burmese plate in NW part of Andaman induced NE- SW and NW- SE trending sutures. The Study aims to validate the orientation of the fault patterns in carbonate rocks through Ground Penetrating Radar. To conduct GPR surveys two cave sites 400 m apart are selected. GPR - SIR-3000 instrument with dipole antenna in bistatic arrangement in reflection mode with stationary point mode is employed. Four depth (time) slices computed from the transect data for 40 MHz antenna with 500 ns range reflected across the cave No. 1 to a length of 19 m reveal bright linear features and intense spots positioned at the depths of 3 m and below 11 m to 18 m and vertical shaft connecting discontinuities are traced to 25 m depth in all plots. Five depth slices at an interval of 4.0 m to a total distance of 28 m with 40 MHz antenna with 400 ns have reflected bright regions at the depths from 8.5 m to 12.5 m and scanning up to depth of 20 m in cave No.2. Seven depth slices by using the 80 MHz antenna with time window of 250 ns across the cave No.2 have reflected to 12.5 m depth, show bright regions with high resolutions at the depth range of 8.5 to 12.5 m. Increase of antenna frequencies with lowering of time range has resolved high resolution reflections of cavities, cracks and reduction of depth in the cave No. 2 than the in cave No. 1. Induction of cracks and fissures in carbonate rocks due to erstwhile tectonic repercussion were subsequently increased their sizes through rain water percolation and dissolution. Depth (time) slices of GPR in all transects across the cave orientations in two sites proved that continuation of caves are aligned in NW-SE and NE-SW directions.
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