Abstract

Remote and extreme regions such as in the Arctic remain a challenging ground for geological mapping and mineral exploration. Coastal cliffs are often the only major well-exposed outcrops, but are mostly not observable by air/spaceborne nadir remote sensing sensors. Current outcrop mapping efforts rely on the interpretation of Terrestrial Laser Scanning and oblique photogrammetry, which have inadequate spectral resolution to allow for detection of subtle lithological differences. This study aims to integrate 3D-photogrammetry with vessel-based hyperspectral imaging to complement geological outcrop models with quantitative information regarding mineral variations and thus enables the differentiation of barren rocks from potential economic ore deposits. We propose an innovative workflow based on: (1) the correction of hyperspectral images by eliminating the distortion effects originating from the periodic movements of the vessel; (2) lithological mapping based on spectral information; and (3) accurate 3D integration of spectral products with photogrammetric terrain data. The method is tested using experimental data acquired from near-vertical cliff sections in two parts of Greenland, in Karrat (Central West) and Søndre Strømfjord (South West). Root-Mean-Square Error of (6.7, 8.4) pixels for Karrat and (3.9, 4.5) pixels for Søndre Strømfjord in X and Y directions demonstrate the geometric accuracy of final 3D products and allow a precise mapping of the targets identified using the hyperspectral data contents. This study highlights the potential of using other operational mobile platforms (e.g., unmanned systems) for regional mineral mapping based on horizontal viewing geometry and multi-source and multi-scale data fusion approaches.

Highlights

  • Near-vertical cliff sections in Arctic regions such as Greenland offer excellent rock exposures, for investigating and characterizing mineral deposits

  • We introduce here a novel and flexible approach for mapping near-vertical cliff sections along fjords, coastlines and valleys in remote regions, which are difficult to map by means of classic geological field campaigns or space-airborne remote sensing surveys

  • To the authors’ best knowledge, this is the first time a vessel is used for acquisition of spectral data from vertical cliffs

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Summary

Introduction

Near-vertical cliff sections in Arctic regions such as Greenland offer excellent rock exposures, for investigating and characterizing mineral deposits. The detailed mapping of lithologies, structures, and the spatial variation of mineral–chemical content is challenging due to the inaccessible nature of alpine, near-vertical topography. To overcome the obstacles of working in inaccessible areas, aerial surveys could be flown deploying either oblique photogrammetric [1,3,4,5,6,7] or light detection and ranging (LiDAR) techniques [8]. Oblique photogrammetry has been exploited in great details in west, east and eastern north Greenland, and the culmination of this has been the production of over 500 km vertical geological sections as well as several map sheets covering Disko, Nuussuaq and Kilen [2,7,10,11,12]

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