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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

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Reference TypeJournal (article/letter/editorial)
TitleThe system Pd-Fe-S at 900 degrees , 725 degrees , 550 degrees , and 400 degrees C
JournalEconomic Geology
AuthorsMakovicky, E.Author
Karup-Moller, S.Author
Year1993 (August 1)Volume88
Issue5
PublisherSociety of Economic Geologists
DOIdoi:10.2113/gsecongeo.88.5.1269Search in ResearchGate
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Mindat Ref. ID227923Long-form Identifiermindat:1:5:227923:1
GUID0
Full ReferenceMakovicky, 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
Plain TextMakovicky, 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
In(1993, August) Economic Geology Vol. 88 (5) Society of Economic Geologists

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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
Karup-Moller, S., Makovicky, E. (1986) The system Pd-Co-S at 1,000 degrees , 800 degrees , 600 degrees , and 400 degrees C. Economic Geology, 81 (5) 1049-1055 doi:10.2113/gsecongeo.81.5.1049
Lusk, John, Scott, Steven D., Ford, Clifford E. (1993) Phase relations in the Fe-Zn-S system to 5 kbars and temperatures between 325 degrees and 150 degrees C. Economic Geology, 88 (7) 1880-1903 doi:10.2113/gsecongeo.88.7.1880
O'Neill, Thomas Francis (1948) The hydrothermal alteration of feldspars at 250 degrees C. to 400 degrees C. Economic Geology, 43 (3) 167-180 doi:10.2113/gsecongeo.43.3.167
Gruner, John Walter (1944) The hydrothermal alteration of feldspars in acid solutions between 300 degrees and 400 degrees C. Economic Geology, 39 (8) 578-589 doi:10.2113/gsecongeo.39.8.578
Roseboom, Eugene H. (1966) An investigation of the system Cu-S and some natural copper sulfides between 25 degrees and 700 degrees C. Economic Geology, 61 (4) 641-672 doi:10.2113/gsecongeo.61.4.641
Clark, T., Naldrett, A. J. (1972) The Distribution of Fe and Ni Between Synthetic Olivine and Sulfide at 900 degrees C. Economic Geology, 67 (7) 939-952 doi:10.2113/gsecongeo.67.7.939
Arnold, R. G. (1962) Equilibrium relations between pyrrhotite and pyrite from 325 degrees to 743 degrees C. Economic Geology, 57 (1) 72-90 doi:10.2113/gsecongeo.57.1.72
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
Maurel, C. (1973) Mechanism of Hydrothermal Sphalerite<-->Galena Replacement at 300 degrees C. Economic Geology, 68 (5) 665-670 doi:10.2113/gsecongeo.68.5.665
Rajamani, V. (1976) Distribution of iron, cobalt, and nickel between synthetic sulfide and orthopyroxene at 900 degrees C. Economic Geology, 71 (4) 795-802 doi:10.2113/gsecongeo.71.4.795
 
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