APPLICATION OF REMOTE SENSING AND AIRBORNE SPECTROMETRIC DATA ANALYSIS TO DELINEATE THE ALTERATION ZONES AT GABAL SUWAYQAT AREA CENTRAL EASTERN DESERT, EGYPT

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Abstract

The present study aims to study the potentiality of promised radioactive zones in the granitic rocks at Gable Suwayqat area. The Processed Landsat ETM+ data false color composite image (FCC) band 7, 4, 2 in RGB, band ratios (5/7, 4/3, 3/1), (5/7, 5/1, 4), (3/1, 5/4,7/5) in red green blue and 5/7 in gray color. Principal component analysis (Pc2, Pc3, Pc5) in RGB were prepared for discriminating rock unites. Verified by the fieldwork and airborne gammaray spectrometric surveyed data enabled to differentiate the acidic and mafic rocks, and identified the alteration zones in the granitic rocks, which were effectively distinguished into high felsic and low ferromagnesian mineral contents, relative to the other granite areas. The gamma-ray spectrometric interpretations reveal that most of radiometric anomalies recorded at north eastern and south western sides of study area. The structural framework and consequent surface features controled and managed the distribution and localization of the radioactive elements and the environmental dose rates in the area. The high fractures density act as good channels and passages for the mineral bearing hydrothermal ascending fluids and the percolating meteoric water that leached uranium mineralization and redeposited it in the adjacent fractured sites. Such processes in the granitic masses may be responsible for the presence of uranium and thorium mineralizations in these granites. The calculated dose rates range between 0.1 and 1.1m Sv/year, indicating that the study area remains safe and under the maximum permissible safe radiation dose rate without harm to the individual, with continuous external irradiation of the whole body. The results show that the target area has some eU, eTh, and K% anomalies related to the biotite granites and are structurally controlled by the dominated faults.
遥感与航空光谱数据分析在埃及中东部沙漠gabal suwayqat地区蚀变带划分中的应用
本研究旨在研究山墙地区花岗岩中潜在放射性带的可能性。处理后的Landsat ETM+数据假彩色合成图像(FCC)波段7,4,2为RGB,波段比率为(5/ 7,4 / 3,3 /1),(5/ 7,5 / 1,4),(3/ 1,5 /4,7/5)为红绿蓝,5/7为灰色。利用RGB主成分分析(Pc2、Pc3、Pc5)对岩石单元进行判别。经野外考察和航空伽玛谱测量资料验证,能够区分酸性岩和基性岩,并识别出花岗岩中的蚀变带,相对于其他花岗岩区,有效区分出高长英质和低镁铁矿物含量。伽玛能谱分析结果表明,研究区东北侧和西南侧记录的辐射异常居多。结构框架和随之而来的表面特征控制和管理着该地区放射性元素的分布和局部以及环境剂量率。高裂缝密度为含矿热液上升流体和大气水渗透提供了良好的通道和通道,使铀矿化在邻近的裂缝部位浸出并重新沉积。花岗岩中的这种过程可能是这些花岗岩中铀和钍矿化的原因。计算出的剂量率范围在0.1 - 1.1m西沃特/年之间,表明研究区域在持续的全身外照射下仍然是安全的,处于最大允许的安全辐射剂量率下,对个人没有伤害。结果表明,靶区存在与黑云母花岗岩有关的eU、eTh和K%异常,受主控断裂的构造控制。
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