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Article

Unravelling the Deformation of Paleoproterozoic Marbles and Zn-Pb Ore Bodies by Combining 3D-Photogeology and Hyperspectral Data (Black Angel Mine, Central West Greenland)

1
Department of Mapping and Mineral Resources, Geological Survey of Denmark and Greenland (GEUS), Øster Voldgade 10, 1350 Copenhagen, Denmark
2
Division Exploration Technology, Helmholtz-Institute Freiberg for Resource Technology (HZDR), Chemnitzer Straße 40, 09599 Freiberg, Germany
3
Geologische Landesuntersuchung GmbH Freiberg, Halsbrücker Str. 34, 09599 Freiberg, Germany
4
G.U.B. Ingenieur AG, Halsbrücker Str. 34, 09599 Freiberg, Germany
*
Author to whom correspondence should be addressed.
Minerals 2022, 12(7), 800; https://doi.org/10.3390/min12070800
Submission received: 25 May 2022 / Revised: 20 June 2022 / Accepted: 20 June 2022 / Published: 23 June 2022
(This article belongs to the Special Issue 3D-Modelling of Crustal Structures and Mineral Deposit Systems)

Abstract

The Black Angel Zn-Pb ore deposit is hosted in folded Paleoproterozoic marbles of the Mârmorilik Formation. It is exposed in the southern part of the steep and inaccessible alpine terrain of the Rinkian Orogen, in central West Greenland. Drill-core data integrated with 3D-photogeology and hyperspectral imagery of the rock face allow us to identify stratigraphic units and extract structural information that contains the geological setting of this important deposit. The integrated stratigraphy distinguishes chemical/mineralogical contrast within lithologies dominated by minerals that are difficult to distinguish with the naked eye, with a similar color of dolomitic and scapolite-rich marbles and calcitic, graphite-rich marbles. These results strengthen our understanding of the deformation style in the marbles and allow a subdivision between evaporite-carbonate platform facies and carbonate slope facies. Ore formation appears to have been mainly controlled by stratigraphy, with mineralizing fluids accumulating within permeable carbonate platform facies underneath carbonate slope facies and shales as cap rock. Later, folding and shearing were responsible for the remobilization and improvement of ore grades along the axial planes of shear folds. The contact between dolomitic scapolite-rich and calcitic graphite-rich marbles probably represents a direct stratigraphic marker, recognizable in the drill-cores, to be addressed for further 3D-modeling and exploration in this area.
Keywords: 3D-photogeology; hyperspectral data; Greenland; Paleoproterozoic; Zn-Pb ore deposits 3D-photogeology; hyperspectral data; Greenland; Paleoproterozoic; Zn-Pb ore deposits

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MDPI and ACS Style

Guarnieri, P.; Thiele, S.T.; Baker, N.; Sørensen, E.V.; Kirsch, M.; Lorenz, S.; Rosa, D.; Unger, G.; Zimmermann, R. Unravelling the Deformation of Paleoproterozoic Marbles and Zn-Pb Ore Bodies by Combining 3D-Photogeology and Hyperspectral Data (Black Angel Mine, Central West Greenland). Minerals 2022, 12, 800. https://doi.org/10.3390/min12070800

AMA Style

Guarnieri P, Thiele ST, Baker N, Sørensen EV, Kirsch M, Lorenz S, Rosa D, Unger G, Zimmermann R. Unravelling the Deformation of Paleoproterozoic Marbles and Zn-Pb Ore Bodies by Combining 3D-Photogeology and Hyperspectral Data (Black Angel Mine, Central West Greenland). Minerals. 2022; 12(7):800. https://doi.org/10.3390/min12070800

Chicago/Turabian Style

Guarnieri, Pierpaolo, Sam T. Thiele, Nigel Baker, Erik V. Sørensen, Moritz Kirsch, Sandra Lorenz, Diogo Rosa, Gabriel Unger, and Robert Zimmermann. 2022. "Unravelling the Deformation of Paleoproterozoic Marbles and Zn-Pb Ore Bodies by Combining 3D-Photogeology and Hyperspectral Data (Black Angel Mine, Central West Greenland)" Minerals 12, no. 7: 800. https://doi.org/10.3390/min12070800

APA Style

Guarnieri, P., Thiele, S. T., Baker, N., Sørensen, E. V., Kirsch, M., Lorenz, S., Rosa, D., Unger, G., & Zimmermann, R. (2022). Unravelling the Deformation of Paleoproterozoic Marbles and Zn-Pb Ore Bodies by Combining 3D-Photogeology and Hyperspectral Data (Black Angel Mine, Central West Greenland). Minerals, 12(7), 800. https://doi.org/10.3390/min12070800

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