Identifying Hydrothermal Alterations Using Singularity Mapping of PCA Images Based on ASTER Data

Abstract

This work integrated selective principal component analysis (SPCA) with a singularity fractal model to map hydrothermal alterations of argillic, phyllic, and propylitic in the north-west of Kerman city in Iran. SPCA results were provided for short wave infrared (SWIR) bands of the Advanced Spaceborne Thermal Emission and Reflection Radiometer (ASTER) sensor to map phyllic and propylitic alterations. Also, the bands 5-7 were applied to map the argillic alteration zone. SPCA results could present useful information for alteration mapping but it does not show the purest pixels of alteration. Therefore, a fractal model of singularity was applied to highlight the different alteration pixels in the Kerman Cenozoic magmatic arc (KCMA). Thus, the singularity index of different hydrothermal alteration zones was produced. Comparing the obtained results with the field data showed that Kader, Serenu, Meiduk, and Abdar deposits were acceptably identified by alteration mapping. Also, it seems that the singularity index could not discriminate the hydrothermal alterations of argillic and phyllic. The same spectral signature of kaolinite and muscovite minerals is the main reason for misclassifications.

Geology, Geochemistry and Geophysical Studies in Exploration of Copper and Iron Reserves: A Case Study

“…In the first geophysical exploration phase in the Hefdah Chenar area, the geoelectric method was performed. Porphyry copper deposits usually show four significant kinds of hydrothermal alterations: potassic, phyllic, argillic, and propylitic [26]. There were high-velocity extended veins and uncertainty of the main mineralization zone around argillic-cercite strip corresponding to granodiorite intrusive mass.…”