Synergy of Remote Sensing Data for Exploring Hydrothermal Mineral Resources Using GIS-Based Fuzzy Logic Approach

被引:20
作者
Abdelkareem, Mohamed [1 ,2 ]
Al-Arifi, Nassir [3 ]
机构
[1] South Valley Univ, Fac Sci, Geol Dept, Qena 83523, Egypt
[2] South Valley Univ, Remote Sensing Lab, Qena 83523, Egypt
[3] King Saud Univ, Geol & Geophys Dept, Chair Nat Hazards & Mineral Resources, Riyadh 68953, Saudi Arabia
关键词
remote sensing; hydrothermal ores; fuzzy logic; Arabian Nubian Shield; CENTRAL EASTERN DESERT; ASTER SWIR DATA; ALTERATION ZONES; PROSPECTIVITY; EXPLORATION; GOLD; DEPOSITS; EXTRACTION; DISTRICT; NEVADA;
D O I
10.3390/rs13224492
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
The Arabian Nubian Shield (ANS) contains a variety of gold deposits in the form of veins and veinlets formed by hydrothermal fluids. Characterizing potential areas of hydrothermal alteration zones therefore provides a significant tool for prospecting for hydrothermal gold deposits. In this study, we develop a model of exploration for hydrothermal mineral resources in an area located in the ANS, Egypt, using multiple criteria derived from Advanced Spaceborne Thermal Emission and Reflection Radiometer (ASTER), Landsat-Operational Land Imager (OLI), and Sentinel-2 data and field work through GIS-based fuzzy logic approach. The hydrothermal alteration zones (HAZs) map extracted from combining mineral indices, spectral bands, and ratios is consistent with observed argillic alteration zones around the mineralized veins. Combining HAZs and lineament density led to identification of six zones based on their mineralization potential, and provides a tool for successful reconnaissance prospecting for future hydrothermal mineral deposits. The detected zones are labeled as excellent, very high, high, moderate, low, and very low, based on their potential for Au production, and the predictive excellent and very high zones cover about 1.6% of the study area. This model also shows that target prospective zones are quartz veins controlled by NNW-SSE trending fracture/fault zones all crosscutting Precambrian rocks of the ANS. Field observations and petrographic and X-ray diffraction analyses were performed to validate the mineral prospective map and revealed that quartz veins consist of gold-sulfide mineralization (e.g., gold, pyrite, chalcopyrite, and sphalerite). Consistency between the high potential hydrothermal alterations zones (HAZs) and the location of gold mineralization is achieved.
引用
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页数:20
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