2016
DOI: 10.1016/j.oregeorev.2016.03.006
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Metallogeny of Greenland

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Cited by 21 publications
(32 citation statements)
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References 234 publications
(493 reference statements)
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“…The nearby Black Angle Pb-Zn deposit is separated from the Nunngarut Peninsula by the smaller Affarlikassaa fjord. The study area belongs to the Mârmorilik Formation, a 1600 m thick carbonate-dominated rock sequence representing the southernmost stratigraphy of the Paleoproterozoic Karrat Group [21]. It was deposited between 2.1 and 1.9 Ga in an epicontinental marginal basin as platform carbonates [21], nonconformably overlies a suite of strong deformed Archean orthogneisses, and is overlain by flysch-type metasedimentary rocks of the Nûkavsak Formation [22].…”
Section: Nunngarut Peninsula Maarmorilik Greenlandmentioning
confidence: 99%
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“…The nearby Black Angle Pb-Zn deposit is separated from the Nunngarut Peninsula by the smaller Affarlikassaa fjord. The study area belongs to the Mârmorilik Formation, a 1600 m thick carbonate-dominated rock sequence representing the southernmost stratigraphy of the Paleoproterozoic Karrat Group [21]. It was deposited between 2.1 and 1.9 Ga in an epicontinental marginal basin as platform carbonates [21], nonconformably overlies a suite of strong deformed Archean orthogneisses, and is overlain by flysch-type metasedimentary rocks of the Nûkavsak Formation [22].…”
Section: Nunngarut Peninsula Maarmorilik Greenlandmentioning
confidence: 99%
“…Locally, interbedded horizons of quartzites, tremolite-rich marbles and possible metamorphosed evaporites in the form of anhydrite occur [21,23]. The Black Angel Mississippi-Valley-Type (MVT) Pb-Zn deposit is emplaced within the Mârmorilik Formation [22,24], causing an overprint of the marbles by basal brines.…”
Section: Nunngarut Peninsula Maarmorilik Greenlandmentioning
confidence: 99%
“…The application of multispectral satellite imagery for mineral prospecting in remote and inaccessible metallogenic provinces is noteworthy for mining companies and the mineral exploration community for reconnaissance stages of systematic exploration projects. Many regions in the High Arctic remain poorly investigated for mineral exploration due to cold climate environments and remoteness, especially the northern part of Greenland containing Zn-Pb and Cu-Au mineralization [1][2][3]. The visible and near-infrared (VNIR), shortwave infrared (SWIR) and thermal infrared (TIR) bands of multispectral remote sensing data contain unprecedented spectral and spatial capabilities for detecting hydrothermal alteration minerals and lithological units associated with a variety of ore mineralization [4][5][6][7][8][9][10][11][12][13][14][15][16][17][18][19][20][21][22].…”
Section: Introductionmentioning
confidence: 99%
“…Inglefield Land is an ice-free region (78 • N-79 • N and 72 • 30 W-66 • W) in northwest Greenland (Figure 1), which contains copper-gold mineralization hosted by garnet-sillimanite paragneiss, orthogneiss, and mafic-ultramafic rocks [1][2][3][50][51][52]. A few geological investigations were carried out in Inglefield Land by the Geological Survey of Denmark and Greenland (GEUS) during years 1994 (an airborne geophysical survey) and 1995 (fieldwork geological mapping, mineralization studies, and a regional stream-sediment geochemical survey).…”
Section: Introductionmentioning
confidence: 99%
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