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Karup-Moller, S., Makovicky, E. (2002) THE SYSTEM Fe Os S AT 1180 , 1100  AND 900 C. The Canadian Mineralogist, 40 (2) 499-507 doi:10.2113/gscanmin.40.2.499

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Reference TypeJournal (article/letter/editorial)
TitleTHE SYSTEM Fe Os S AT 1180 , 1100  AND 900 C
JournalThe Canadian Mineralogist
AuthorsKarup-Moller, S.Author
Makovicky, E.Author
Year2002 (April 1)Volume40
Issue2
PublisherMineralogical Association of Canada
Download URLhttps://rruff.info/doclib/cm/vol40/CM40_499.pdf+
DOIdoi:10.2113/gscanmin.40.2.499Search in ResearchGate
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Mindat Ref. ID63632Long-form Identifiermindat:1:5:63632:2
GUID0
Full ReferenceKarup-Moller, S., Makovicky, E. (2002) THE SYSTEM Fe Os S AT 1180 , 1100  AND 900 C. The Canadian Mineralogist, 40 (2) 499-507 doi:10.2113/gscanmin.40.2.499
Plain TextKarup-Moller, S., Makovicky, E. (2002) THE SYSTEM Fe Os S AT 1180 , 1100  AND 900 C. The Canadian Mineralogist, 40 (2) 499-507 doi:10.2113/gscanmin.40.2.499
In(2002, April) The Canadian Mineralogist Vol. 40 (2) Mineralogical Association of Canada

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Makovicky, E., Makovicky, M., Rose-Hansen, J. (2002) THE SYSTEM Fe Rh S AT 900  AND 500 C. The Canadian Mineralogist, 40 (2) 519-526 doi:10.2113/gscanmin.40.2.519
Majzlan, J., Makovicky, M., Makovicky, E., Rose-Hansen, J. (2002) THE SYSTEM Fe Pt S AT 1100 C. The Canadian Mineralogist, 40 (2) 509-517 doi:10.2113/gscanmin.40.2.509
Karup-Moller, S., Makovicky, E. (2007) THE SYSTEM Cu-Rh-S AT 900 , 700 , 540  AND 500 C. The Canadian Mineralogist, 45 (6) 1535-1542 doi:10.3749/canmin.45.6.1535
Makovicky, E., Karup-Moller, S. (1993) The system Pd-Fe-S at 900 degrees , 725 degrees , 550 degrees , and 400 degrees C. Economic Geology, 88 (5) 1269-1278 doi:10.2113/gsecongeo.88.5.1269
Makovicky, E., Tippelt, G., Forcher, K., Lottermoser, W., Karup-Moller, S., Amthauer, G. (2003) MOSSBAUER STUDY OF Fe-BEARING SYNTHETIC TENNANTITE. The Canadian Mineralogist, 41 (5) 1125-1134 doi:10.2113/gscanmin.41.5.1125
Ueno, T., Scott, S. D. (2002) PHASE EQUILIBRIA IN THE SYSTEM Zn Fe Ga S AT 900  AND 800 C. The Canadian Mineralogist, 40 (2) 563-570 doi:10.2113/gscanmin.40.2.563
Karup-Møller, S., & Makovicky, E. (2007). THE SYSTEM Cu–Rh–S AT 900°, 700°, 540° AND 500° C. The Canadian Mineralogist, 45(6), 1535-1542.
Karup-Moller, S., Makovicky, E. (1993) The system Pd-Ni-S at 900 degrees , 725 degrees , 550 degrees , and 400 degrees C. Economic Geology, 88 (5) 1261-1268 doi:10.2113/gsecongeo.88.5.1261
Hem, S. R., Makovicky, E. (2004) The System Fe-Co-Ni-As-S. II. Phase Relations in the (Fe,Co,Ni)As1.5S0.5 Section at 650° and 500°C. The Canadian Mineralogist, 42 (1). 63-86 doi:10.2113/gscanmin.42.1.63
Hem, S. R., Makovicky, E. (2004) THE SYSTEM Fe-Co-Ni-As-S. I. PHASE RELATIONS IN THE (Fe,Co,Ni)As0.5S1.5 SECTION AT 650° AND 500°C. The Canadian Mineralogist, 42 (1). 43-62 doi:10.2113/gscanmin.42.1.43
Makovicky, Emil, Karup-Møller, Sven (2016) THE Pd–Ni–Fe–s Phase System At 550 and 400 °C. The Canadian Mineralogist, 54 (2) 377-400 doi:10.3749/canmin.1500016
 
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