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Thus, the methods used to extract information from hyperspectral data must be adjusted to fit the local conditions and minimize these effects. The aim of the study is to: Materials and Methods For the method of integrating hyperspectral horizontal scanning with high-oblique to near-horizontal photogrammetry to be robust, it should be able to cope with data acquired at different angles and distances from different platforms.

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The method is therefore implemented and tested with terrain data point cloud generated from: To integrate the terrain and hyperspectral datasets, the generated 3D point cloud is projected and rasterized to identical perspective as the hyperspectral scans. A key process step in the workflow, after correction of the hyperspectral data for the periodic movements of the vessel, is to find corresponding points between the two image sets. To achieve this, the georeferencing step in the MEPHySTo toolbox [ 45 ] developed for drone-borne nadir viewing angle is modified and adapted for horizontal scanning. A 3D interpretation and quantification of geology along the topography is then possible based on these products.

Study Area and Geological Setting We selected two remote areas of Greenland that are currently under-explored due to poor accessibility but have a high mineral potential. The Karrat area in West Greenland Figure 1 a is characterized by rugged alpine terrain that in many areas is difficult to access. The morphology here is Inside view of russian dating from australian perspective. Highlights by E—W trending, deeply incised fjords with 1 to 1. Rocks exposed along these cliffs are made up of Archean basement and Early Paleoproterozoic siliciclastic and carbonate sequences of the Karrat Group [ 4647 ]. The Archean basement comprises leucocratic orthogneiss, deformed during multiple orogenic events [ 48 ].

The Karrat Group was deposited in a shelf environment with turbiditic sequences and carbonate platforms. The Karrat Group sequence shows greenschist to amphibolite facies metamorphism [ 48 ]. The whole succession of Archean basement and Karrat Group meta-sediments was later overthrusted by Archean basement-cored nappes during the NW—SE directed compressional Rinkian event [ 46 ]. The SNO consists predominantly of Archaean gneisses that were reworked under amphibolite to granulite-facies conditions during orogeny [ 49 ]. The host rocks for the dyke swarm are mainly tonalitic and granodioritic gneisses.

The construction of a tectonic structural model describing the geological development of the Kangerlussuaq area remains challenging and the use of virtual outcrops based on hyperspectral imaging systems HSI is fundamental. The rapidity of HSI acquisition on a vessel allows one to provide valuable information that delivers not only lithological constraints but also structural control. They proposed that the area has undergone several episodes of deformation. Prior research in the study area of interest has mainly been based on lineament mapping and the extension of limited field observations.

Not only is this work tedious but also implies numerous assumptions due to the limited extent of in-situ data and the different scales of observation. Our approach provides an access to the third dimension to these studies mostly based on maps. The use of vertical cliffs allows a better constraint of the 3D geometry of those complex structures. Data Acquisition Several vessel-based hyperspectral scans were acquired along the coastline of Kirgasima peninsula while sailing from Kangerluarsuk to Inukassaat Fjord and in the Karrat region in August to complement existing Digital Outcrop Models with quantitative information about mineral variations [ 48 ] Figure 1 a.

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