Kristoffer Szilas

[26] Gardiner, N., Johnson, T.E., Kirkland, C., Szilas, K. (2018). Modelling the Hafnium–Neodymium Evolution of Early Earth: A Study from West Greenland. Journal of Petrology (in press).

[25] van Hinsberg, V., Crotty, C., Roozen, S., Szilas, K., Kisters, A. (2018). Pressure–Temperature History of the >3 Ga Tartoq Greenstone Belt in Southwest Greenland and Its Implications for Archaean Tectonics. Geosciences 8, 367.

[24]  Guotana, J.M., Morishita, T., Yamaguchi, R., Nishio, I., Tamura, A., Tani, K., Harigane, Y., Szilas, K., Pearson, D.G. (2018). Contrasting Textural and Chemical Signatures of Chromitites in the Mesoarchaean Ulamertoq Peridotite Body, Southern West Greenland. Geosciences 8, 328.

[23]  Kirkland, C.L., Yakymchuk, C., Szilas, K., Evans, N., Hollis, J., McDonald, B., Gardiner, N. (2018). Apatite; a U-Pb thermochronometer or geochronometer? Lithos 318, 143-147.

[22]  Szilas, K. (2018). A Geochemical Overview of Mid-Archaean Metavolcanic Rocks from Southwest Greenland. Geosciences 8, 266.

[21]  Yakymchuk, C. & Szilas, K. (2018). Corundum formation by metasomatic reactions in Archean metapelite, SW Greenland - Exploration vectors for ruby deposits within high-grade greenstone belts. Geoscience Frontiers 9, 727-749.

[20]  Szilas, K., van Hinsberg, V.J., McDonald, I., Næraa, T., Rollinson, H., Adetunji, J. & Bird, D. (2018). Highly refractory Archaean peridotite cumulates:  Petrology and geochemistry of the Seqi Ultramafic Complex, SW Greenland. Geoscience Frontiers 9, 689-714.

[19]  Klausen, M.B., Szilas, K., Kokfelt, T.F., Keulen, N., Schumacher, J.C. & Berger, A. (2017). Tholeiitic to calc-alkaline metavolcanic transition in the Archean Nigerlikasik Supracrustal Belt, SW Greenland. Precambrian Research 302, 50-73.

[18]  Rollinson, H., Adetunji J., Lenaz, D. & Szilas, K. (2017). Archaean chromitites show constant Fe3+/ΣFe in Earth´s asthenospheric mantle since 3.8 Ga. Lithos 282, 316-325.

[17]  Szilas, K., Tusch, J., Hoffmann, J.E., Garde, A.A. & Münker, C. (2017). Hafnium isotope constraints on the origin of Mesoarchaean andesites in southern West Greenland, North Atlantic craton. In: Halla, J., Whitehouse, M.J., Ahmad, T. & Bagai, Z. (Eds.) Crust-Mantle Interactions and Granitoid Diversification: Insights from Archaean Cratons. Geological Society, London, Special Publications 449, 19-38.

[16]  Szilas, K., Hoffmann, J.E., Schulz T., Hansmeier, C., Polat, A., Viehmann, S., Kasper, H.U.  & Münker, C. (2016). Combined bulk-rock Hf- and Nd-isotope compositions of Mesoarchaean metavolcanic rocks from the Ivisaartoq Supracrustal Belt, SW Greenland: Deviations from the mantle array caused by crustal recycling. Chemie der Erde 76, 543-554.

[15]  Szilas, K., Maher, K. & Bird, D. (2016). Aluminous gneiss derived by weathering of basaltic source rocks in the Neoarchean Storø Supracrustal Belt, southern West Greenland. Chemical Geology 441, 63-80. 

[14]  Szilas, K., Hoffmann, J.E., Hansmeier, C., Hollis, J.A., Münker, C., Viehmann, S. & Kasper, H.U. (2015). Sm-Nd and Lu-Hf isotope and trace-element systematics of Mesoarchaean amphibolites, inner Ameralik fjord, southern West Greenland. Mineralogical Magazine 79, 857-876.

[13]  Szilas, K., Kelemen, P.B. & Rosing, M.T. (2015). The petrogenesis of ultramafic rocks in the >3.7 Ga Isua supracrustal belt, southern West Greenland: Geochemical evidence for two distinct magmatic cumulate trends. Gondwana Research 28, 565-580.

[12]  Szilas, K., Kelemen, P.B.& Bernstein, S. (2015). Peridotite enclaves hosted by Mesoarchaean TTG-suite orthogneisses in the Fiskefjord region of southern West Greenland. GeoResJ 7, 22-34.

[11]  Keulen, N., Schumacher, J.C., Næraa, T., Kokfelt, T.F., Scherstén, A., Szilas, K., van Hinsberg, V.J., Schlatter, D.M. & Windley, B.F. (2014). Meso- and Neoarchaean geological history of the Bjørnesund and Ravns Storø Supracrustal Belts, southern West Greenland: settings for gold enrichment and corundum formation. Precambrian Research 254, 36-58.

[10]  Szilas, K., van Gool, J.A.M., Scherstén, A. & Frei, R. (2014). The Neoarchaean Storø Supracrustal Belt, Nuuk region, southern West Greenland: An arc-related basin with continent-derived sedimentation. Precambrian Research 247, 208-222.

[9]  Szilas, K., van Hinsberg, V.J., Creaser, R.A. & Kisters, A.F.M. (2014). The geochemical composition of serpentinites in the Mesoarchaean Tartoq Group, SW Greenland: Harzburgitic cumulates or melt-modified mantle? Lithos 198, 103-116.

[8]  Szilas, K., Hoffmann, J.E., Scherstén, A., Kokfelt, T.F. & Münker, C. (2013). Archaean andesite petrogenesis: Insights from the Grædefjord Supracrustal Belt, southern West Greenland. Precambrian Research 236, 1-15.

[7]  Szilas, K. & Garde, A.A. (2013). Mesoarchaean aluminous rocks at Storø, southern West Greenland: New age data and evidence of premetamorphic seafloor weathering of basalts. Chemical Geology 354, 124-138.

[6]  Bernstein, S., Szilas, K. & Kelemen, P.B. (2013). Highly depleted cratonic mantle in West Greenland extending into diamond stability field in the Proterozoic. Lithos 168, 160-172.

[5]  Szilas, K., van Hinsberg, V.J., Kisters, A.F.M., J. Hoffmann, E., Windley, B.F., Kokfelt, T.F., Scherstén, A., Frei, R., Rosing, M.T. & Münker, C. (2013). Remnants of arc-related Mesoarchaean oceanic crust in the Tartoq Group, SW Greenland. Gondwana Research 23, 436-451.

[4]  Kisters, A.F.M., van Hinsberg, V.J. & Szilas, K. (2012). Geology of an Archaean accretionary complex - The structural record of burial and return flow in the Tartoq Group of South West Greenland. Precambrian Research 220, 107-122.

[3]  Szilas, K., Hoffmann, J.E., Scherstén, A., Rosing, M.T., Kokfelt, T.F., Windley, B.F., van Hinsberg, V.J., Næraa, T., Keulen, N., Frei, R. & Münker, C. (2012). Complex calc-alkaline volcanism recorded in Mesoarchaean supracrustal belts north of Frederikshåb Isblink, southern West Greenland: Implications for subduction zone processes in the early Earth. Precambrian Research 208, 90-123.

[2]  Szilas, K., Næraa, T., Scherstén, A., Stendal, H., Frei, R., van Hinsberg, V.J., Kokfelt, T.F. & Rosing, M.T. (2012). Origin of Mesoarchaean arc related rocks with boninite/komatiite affinities from southern West Greenland. Lithos 144, 24-39.

[1]  Scherstén, A., Szilas, K., Creaser, R.A., van Gool, J.A.M., Næraa, T. & Østergaard, C. (2012). Re-Os and U-Pb constraints on gold mineralisation events in the Meso- to Neoarchaean Storø greenstone belt, Storø, southern West Greenland. Precambrian Research 200, 149-162.