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Makovicky, Emil, Karup-Møller, Sven (1995) The system Pd-Fe-Ni-S at 900 and 725°C. Mineralogical Magazine, 59 (397) 685-702 doi:10.1180/minmag.1995.059.397.11

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Reference TypeJournal (article/letter/editorial)
TitleThe system Pd-Fe-Ni-S at 900 and 725°C
JournalMineralogical MagazineISSN0026-461X
AuthorsMakovicky, EmilAuthor
Karup-Møller, SvenAuthor
Year1995 (December)Volume59
Issue397
PublisherMineralogical Society
Download URLhttps://rruff.info/doclib/MinMag/Volume_59/59-397-685.pdf+
DOIdoi:10.1180/minmag.1995.059.397.11Search in ResearchGate
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Mindat Ref. ID2698Long-form Identifiermindat:1:5:2698:1
GUID0
Full ReferenceMakovicky, Emil, Karup-Møller, Sven (1995) The system Pd-Fe-Ni-S at 900 and 725°C. Mineralogical Magazine, 59 (397) 685-702 doi:10.1180/minmag.1995.059.397.11
Plain TextMakovicky, Emil, Karup-Møller, Sven (1995) The system Pd-Fe-Ni-S at 900 and 725°C. Mineralogical Magazine, 59 (397) 685-702 doi:10.1180/minmag.1995.059.397.11
In(1995, December) Mineralogical Magazine Vol. 59 (397) Mineralogical Society
Abstract/NotesAbstractThe system Pd-Fe-Ni-S was studied at 900 and 725°C by means of dry condensed charges. At both temperatures it is dominated by the phase relationships involving sulphide melt. Pd-Fe-Ni alloys with broad miscibility primarily coexist with the melt; they are relatively enriched in Pd, whereas the associated melt is enriched in Ni. With decreasing temperature the melt recedes from Fe-rich regions. The incompatibility of PdS (extensive solid solution with Ni) and mss at 900°C is replaced by their co-crystallization (± disulphide(s) of Ni,Fe or ± sulphide melt) at 725°C The Ni/Fe ratio in the melt changes regularly against that in mss with increasing S fugacity and Pd contents in these two phases. (Ni,Fe)3±xS2 and Pd4S play important roles at 725°C. The data offer an array of distribution coefficients and solubility values suitable for geological interpretations.

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Karup-Møller, S., Makovicky, E., Barnes, S.-J. (2008) The metal-rich portions of the phase system Cu-Fe-Pd-S at 1000°C, 900°C and 725°C: implications for mineralization in the Skaergaard intrusion. Mineralogical Magazine, 72 (4) 941-951 doi:10.1180/minmag.2008.072.4.941
Makovicky, E., Karup-Møller, S. (1999) The phase system Fe-Ir-S at 1100, 1000 and 800°C. Mineralogical Magazine, 63 (3) 379-385 doi:10.1180/minmag.1999.063.3.09
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
Makovicky, Emil, Karup-Møller, Sven (2020) The central portions of the Cu–Fe–Se phase system at temperatures from 900 to 300 °C. The Canadian Mineralogist, 58 (2). 203-221 doi:10.3749/canmin.1900071
Makovicky, E., Karup-Møller, S. (2000) Phase relations in the metal-rich portions of the phase system Pt-Ir-Fe-S at 1000°C and 1100°C. Mineralogical Magazine, 64 (6) 1047-1056 doi:10.1180/002646100550047
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
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
Makovicky, Emil, Karup-Møller, Sven (2017) Exploratory studies of the Cu–Pd–Se system at 650°C, 550°C, 400°C, and 300°C. European Journal of Mineralogy, 29 (4) 645-652 doi:10.1127/ejm/2017/0029-2651
Makovicky, Emil, Karup-M�ller, Sven, Makovicky, Milota, Rose-Hansen, Jhon (1990) Experimental studies on the phase systems Fe-Ni-Pd-S and Fe-Pt-Pd-As-S applied to PGE deposits. Mineralogy and Petrology, 42 (1) 307-319 doi:10.1007/bf01162697
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.
(1995) Errata. Mineralogical Magazine, 59 (397) doi:10.1180/minmag.1995.059.397.33
 
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