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M�kinen, Jari, Makkonen, Hannu V. (2004) Petrology and structure of the Palaeoproterozoic (1.9�Ga) Rytky nickel sulphide deposit, Central Finland: a comparison with the Kotalahti nickel deposit. Mineralium Deposita, 39 (4) 405-421 doi:10.1007/s00126-004-0413-4

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Reference TypeJournal (article/letter/editorial)
TitlePetrology and structure of the Palaeoproterozoic (1.9�Ga) Rytky nickel sulphide deposit, Central Finland: a comparison with the Kotalahti nickel deposit
JournalMineralium Deposita
AuthorsM�kinen, JariAuthor
Makkonen, Hannu V.Author
Year2004 (August)Volume39
Issue4
PublisherSpringer Science and Business Media LLC
DOIdoi:10.1007/s00126-004-0413-4Search in ResearchGate
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Mindat Ref. ID156721Long-form Identifiermindat:1:5:156721:6
GUID0
Full ReferenceM�kinen, Jari, Makkonen, Hannu V. (2004) Petrology and structure of the Palaeoproterozoic (1.9�Ga) Rytky nickel sulphide deposit, Central Finland: a comparison with the Kotalahti nickel deposit. Mineralium Deposita, 39 (4) 405-421 doi:10.1007/s00126-004-0413-4
Plain TextM�kinen, Jari, Makkonen, Hannu V. (2004) Petrology and structure of the Palaeoproterozoic (1.9�Ga) Rytky nickel sulphide deposit, Central Finland: a comparison with the Kotalahti nickel deposit. Mineralium Deposita, 39 (4) 405-421 doi:10.1007/s00126-004-0413-4
In(2004, August) Mineralium Deposita Vol. 39 (4) Springer Science and Business Media LLC

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M�kinen, Jari, Makkonen, Hannu V. (2004) Petrology and structure of the Palaeoproterozoic (1.9�Ga) Rytky nickel sulphide deposit, Central Finland: a comparison with the Kotalahti nickel deposit. Mineralium Deposita, 39 (7) 793 doi:10.1007/s00126-004-0445-9
Makkonen, Hannu V.; Mäkinen, Jari; Kontoniemi, Olavi (2008) Geochemical discrimination between barren and mineralized intrusions in the Svecofennian (1.9 Ga) Kotalahti Nickel Belt, Finland. Ore Geology Reviews, 33 (1). doi:10.1016/j.oregeorev.2006.05.011
Hill, R. E. T., Barnes, S. J., Dowling, S. E., Thordarson, T. (2004) Komatiites and nickel sulphide orebodies of the Black Swan area, Yilgarn Craton, Western Australia. 1. Petrology and volcanology of host rocks. Mineralium Deposita, 39 (7) 684-706 doi:10.1007/s00126-004-0437-9
Shalaby, Ibrahim M., Stumpfl, Eugen, Helmy, Hassan M., El Mahallawi, Mahmoud M., Kamel, Omar A. (2004) Silver and silver-bearing minerals at the Um Samiuki volcanogenic massive sulphide deposit, Eastern Desert, Egypt. Mineralium Deposita, 39 (5) 608-621 doi:10.1007/s00126-004-0427-y
Barnes, Stephen J., Fiorentini, Marco L., Fardon, Michael C. (2012) Platinum group element and nickel sulphide ore tenors of the Mount Keith nickel deposit, Yilgarn Craton, Australia. Mineralium Deposita, 47 (1) 129-150 doi:10.1007/s00126-011-0348-5
Watmuff, I.G. (1974) Supergene alteration of the Mt Windarra nickel sulphide ore deposit, Western Australia. Mineralium Deposita, 9 (3) doi:10.1007/bf00203996
Barnes, Stephen J. (2004) Komatiites and nickel sulfide ores of the Black Swan area, Yilgarn Craton, Western Australia. 4. Platinum group element distribution in the ores, and genetic implications. Mineralium Deposita, 39 (7) 752-765 doi:10.1007/s00126-004-0440-1
Barnes, S. J. (2004) Introduction to nickel sulfide orebodies and komatiites of the Black Swan area, Yilgarn Craton, Western Australia. Mineralium Deposita, 39 (7) 679-683 doi:10.1007/s00126-004-0436-x
Bergstøl, S., Vokes, F.M. (1974) Stromeyerite and mckinstryite from the Godejord polymetallic sulphide deposit, central Norweigan Caledonides. Mineralium Deposita, 9 (4) doi:10.1007/bf00206635
Makkonen, Hannu V., , , Tuisku, Pekka, , (2020) Geology and crystallization conditions of the Särkiniemiintrusion and related nickel-copper ore, central Finland – implications for depth of emplacement of 1.88 Ga nickel-bearing intrusions. Bulletin of the Geological Society of Finland, 92 (2) 111-130 doi:10.17741/bgsf/92.2.003
Agnew, Michael W., Large, Ross R., Bull, Stuart W. (2005) Lewis Ponds, a hybrid carbonate and volcanic-hosted polymetallic massive sulphide deposit, New South Wales, Australia. Mineralium Deposita, 39 (8) 822-844 doi:10.1007/s00126-004-0456-6
 
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