基于PRISMA和Sentinel-2A卫星图像的Alma inlier和Fouanou向斜铜蚀变矿物填图及识别

IF 3.3 Q2 MULTIDISCIPLINARY SCIENCES
Ilham M’hamdi Alaoui , Ahmed Akhssas , Anas Bahi , Hassan Ibouh , Saloua Mnissar Himyari , Hicham Khebbi , Fatima Zahra Sbabou
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引用次数: 0

摘要

摩洛哥西部的Anti-Atlas拥有复杂的铜矿床,其起源存在争议,并提出了多种地球动力学模型。该研究首次应用于Alma盆地和Fouanou向斜,将PRISMA (precursour IperSpettrale della Missione Applicativa)图像与Sentinel-2A多光谱数据相结合,以较高的空间和光谱精度准确识别铜相关蚀变矿物,绘制构造线。PRISMA数据集采用了一系列图像处理技术,包括最小噪声分数(MNF)、像素纯度指数(PPI)、n维可视化器(n-Dimensional Visualizer)和光谱角度映射器(SAM),以分离和识别与蚀变相关的矿物。同时,利用主成分分析(PCA)和方向滤波器从Sentinel-2A图像中提取构造轮廓,实现构造特征的精确映射。通过研究区内的三个地质剖面进行了现场验证,并使用手持式光谱仪验证了蚀变带。然后将从PRISMA获得的光谱特征与现场测量结果和USGS光谱库进行比较和验证,以确保矿物学准确性。主要蚀变矿物为孔雀石、蓝铜矿、赤铁矿和针铁矿,具有氧化和表生富集特征。构造分析显示NE-SW ~ ENE-WSW向构造,与泛非构造一致。蚀变晕与主要断裂带的空间对比表明,热液流体循环在成矿过程中发挥了重要作用,特别是在前寒武纪基底与上覆古生代盖层接触的过程中。这些观察结果证明了PRISMA在偏远和地质复杂地区具有成本效益的铜勘探价值。这种综合方法不仅提供了一种可行的勘探策略,而且对西反阿特拉斯的成矿演化提供了新的认识,有助于对其构造-岩浆历史的持续争论,对世界上类似的成矿省具有指导意义。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Tectonic lineament mapping and identification of copper alteration minerals using PRISMA and Sentinel-2A satellite imagery in Alma inlier and Fouanou syncline (western Anti-Atlas, Morocco)
The western Anti-Atlas of Morocco hosts complex copper deposits with debated origins and multiple proposed geodynamic models. This study, applied for the first time to the Alma inlier and the Fouanou syncline, integrates PRecursore IperSpettrale della Missione Applicativa (PRISMA) imagery with Sentinel-2A multispectral data to accurately identify copper-related alteration minerals and map structural lineaments with high spatial and spectral precision. A series of image processing techniques were applied to the PRISMA dataset, including Minimum Noise Fraction (MNF), Pixel Purity Index (PPI), n-Dimensional Visualizer, and Spectral Angle Mapper (SAM), to isolate and identify minerals associated with alteration. In parallel, structural lineaments were extracted from Sentinel-2A imagery using Principal Component Analysis (PCA) and directional filters, enabling the precise mapping of tectonic features. Field validation was carried out through three geological cross-sections within the study area, where alteration zones were verified using a handheld spectrometer. The spectral signatures obtained from PRISMA were then compared and validated against field measurements and the USGS spectral library to ensure mineralogical accuracy. The main alteration minerals identified include malachite, azurite, hematite, and goethite, indicative of oxidation and supergene enrichment. Structural analyses revealed NE-SW to ENE-WSW oriented lineaments, consistent with Pan-African tectonic structures. The spatial correlation between alteration halos and major fault zones suggests that hydrothermal fluid circulation played a significant role in ore deposition, especially along the contact between the Precambrian basement and the overlying Paleozoic cover. These observations demonstrate PRISMA's value for cost-effective copper exploration in remote and geologically complex areas. This integrative methodology provides not only a viable exploration strategy but also offers new insights into the metallogenic evolution of the western Anti-Atlas and contributes to the ongoing debate on its tectono-magmatic history, with implications for similar metallogenic provinces across the world.
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来源期刊
Scientific African
Scientific African Multidisciplinary-Multidisciplinary
CiteScore
5.60
自引率
3.40%
发文量
332
审稿时长
10 weeks
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