Abstract

The gold (Au) geochemical anomaly is an important indicator of gold mineralization. While the traditional field geochemical exploration method is time-consuming and expensive, the hyperspectral remote sensing technique serves as a robust technique for the delineation and mapping of hydrothermally altered and weathered mineral deposits. Nonetheless, mineralization element anomaly detection was still seldomly used in previous hyperspectral remote sensing applications in mineralization. This study explored the coupling relationship between Gaofen-5 (GF-5) hyperspectral data and Au geochemical anomalies through several models. The Au geochemical anomalies in the Chahuazhai mining area, Qiubei County, Yunnan Province, SW China, was studied in detail. First, several noise reduction methods including radiometric calibration, Fast Line-of-sight Atmospheric Analysis of Spectral Hypercubes (FLAASH), Savitzky–Golay filter, and endmember choosing methods including Minimum Noise Fraction (MNF) transformation, matched filtering, and Fast Fourier Transform (FFT) transformation were applied to the Gaofen-5 (GF-5) hyperspectral data processing. The Spectrum-Area (S-A) method was introduced to build an FFT filter to highlight the spectral abnormal characteristics associated with Au geochemical anomaly information. Specifically, the Matched Filtering (MF) technique was applied to the dataset to find the Au geochemical anomaly abundances of endmembers with innovative large-sample learning. Then, Multiple Linear Regression (MLR), Partial Least Squares (PLS) regression, a Back Propagation (BP) network, and Geographically Weighted Regression (GWR) were used to reveal the coupling relationship between the spectra of the processed hyperspectral data and the Au geochemical anomalies. The results show that the GWR analysis has a much higher coefficient of determination, which implies that the Au geochemical anomalies and the spectral information are highly related to spatial locations. GWR works especially well for showing the regional Au geochemical anomaly trend and simulating the Au concentrated areas. The GWR model with application of the S-A method is applicable to the detection of Au geochemical anomalies, which could provide a potential method for Au deposit exploration using GF-5 hyperspectral data.

Highlights

  • Au geochemical element anomaly is a strong indicator of gold mineralization [1,2,3]

  • After applying endmember choosing methods to the GF-5 hyperspectral data, the Geographically Weighted Regression (GWR) model showed high R2 and low root-mean-square deviation (RMSE) between the raster value of points of the GF-5 image processed after inverse Fast Fourier Transform (FFT) and Au content

  • The study showed that hyperspectral data are able to identify the rocks associated with Au mineralization and characterize the mineralogy and mineral chemistry of complex minerals, but can be applied to extract Au geochemical anomalies, which are a strong indicator of gold mineralization, especially Carlin-type gold deposit

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Summary

Introduction

Au geochemical element anomaly is a strong indicator of gold mineralization [1,2,3]. Geochemical exploration of geochemical anomalies associated with Au was useful for the identification, target prediction and prospecting of gold mineralization [4,5]. Au geochemical anomalies are an especially important indicator for tracing Carlin-type gold mineralization, since the Au element often occurs as visible gold in association with sulfides in Carlin-type deposits [6] that are commonly distributed around extensional fault structures and on the margins of isolated platforms and basins and are spatially related to anticlines or second-order faults controlled by regional fault zones [7,8,9,10,11]. The metallogenic age of the “Golden Triangle” Carlin-like gold deposits in Yunnan and Guizhou is in the Late

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