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Remote sensing analysis of geological structures in Peninsular Malaysia using PALSAR data

机译:利用PALSAR数据对马来西亚半岛的地质构造进行遥感分析

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Advances in remote sensing technology allow the application of Synthetic Aperture Radar (SAR) data in geological structural analysis for tropical environments. In this investigation, the Phased Array type L-band Synthetic Aperture Radar (PALSAR) satellite remote sensing data were used to analyze major geological structures in Peninsular Malaysia and provide detailed characterization of lineaments and form-lines in the Bentong-Raub Suture Zone (BRSZ) of Peninsular Malaysia, as well as its implication for sediment-hosted/orogenic gold exploration in tropical environments. Major transcrustal lineaments such as the Bentong-Raub Suture Zone (BRSZ) and Lebir Fault Zone, ductile deformation related to crustal shortening, brittle disjunctive structures (faults and fractures) and collisional mountain range (Main Range Granites) were detected at regional scale using PALSAR ScanSAR data. The major geological structure directions of the BRSZ are N-S, NNE-SSW, NE-SW and NW-SE, which derived from directional filtering analysis to PALSAR fine and polarimetric data. The pervasive array of N-S faults in the study area and surrounding terrain is mainly linked to the N-S trending of the Suture Zone. N-S striking lineaments are often cut by younger NE-SW and NW-SE-trending lineaments. Gold mineralized trends lineaments are associated with the intersection of N-S, NE-SW, NNW-SSE and ESE-WNW faults and curvilinear features in shearing and alteration zones. Lineament analysis on PALSAR satellite remote sensing data is a useful tool for detecting the boundary between the Gondwana-derived terranes and major geological features associated with suture zone especially for inaccessible regions in tropical environments.
机译:遥感技术的进步允许将合成孔径雷达(SAR)数据应用于热带环境的地质结构分析中。在这项调查中,相控阵型L波段合成孔径雷达(PALSAR)卫星遥感数据用于分析马来西亚半岛的主要地质结构,并详细描述了Bentong-Raub缝合带(BRSZ)的构造和构造线),以及其对热带环境中沉积物/造山带金矿勘探的意义。使用PALSAR在区域范围内检测到主要的跨壳地层,例如Bentong-Raub缝合带(BRSZ)和Lebir断裂带,与地壳缩短相关的韧性变形,脆性分离结构(断层和裂缝)和碰撞山脉(主要山脉花岗岩)。 ScanSAR数据。 BRSZ的主要地质构造方向是N-S,NNE-SSW,NE-SW和NW-SE,这是通过对PALSAR精细和极化数据进行定向过滤分析得出的。研究区和周围地形中广泛分布的N-S断层主要与缝合带的N-S趋势有关。 N-S震撼的风格通常被年轻的NE-SW和NW-SE趋势的风格所削减。金矿化趋势线与剪切,蚀变带的N—S,NE—SW,NNW—SSE和ESE—WNW断层的交汇点和曲线特征有关。对PALSAR卫星遥感数据进行的线质分析是检测冈瓦纳衍生的地形和与缝合带有关的主要地质特征之间的边界的有用工具,特别是对于热带环境中无法访问的区域。

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