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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

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Reference TypeJournal (article/letter/editorial)
TitleEquilibrium relations between pyrrhotite and pyrite from 325 degrees to 743 degrees C
JournalEconomic Geology
AuthorsArnold, R. G.Author
Year1962 (January 1)Volume57
Issue1
PublisherSociety of Economic Geologists
DOIdoi:10.2113/gsecongeo.57.1.72Search in ResearchGate
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Mindat Ref. ID232176Long-form Identifiermindat:1:5:232176:3
GUID0
Full ReferenceArnold, 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
Plain TextArnold, 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
In(1962, January) Economic Geology Vol. 57 (1) Society of Economic Geologists

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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
Wood, Scott A., Crerar, David A., Borcsik, Maria P. (1987) Solubility of the assemblage pyrite-pyrrhotite-magnetite-sphalerite-galena-gold-stibnite-bismuthinite-argen- tite-molybdenite in H 2 O-NaCl-CO 2 solutions from 200 degrees to 350 degrees C degrees. Economic Geology, 82 (7) 1864-1887 doi:10.2113/gsecongeo.82.7.1864
Arnold, R. G., Coleman, R. G., Fryklund, V. C. (1962) Temperature of crystallization of pyrrhotite and sphalerite from the Highland-Surprise Mine, Coeur d'Alene district, Idaho. Economic Geology, 57 (8) 1163-1174 doi:10.2113/gsecongeo.57.8.1163
Arnold, R. G., Malik, O. P. (1975) The NiS-S system above 980 degrees C; a revision. Economic Geology, 70 (1) 176-182 doi:10.2113/gsecongeo.70.1.176
Clark, Bruce R., Kelly, William C. (1973) Sulfide Deformation Studies; I, Experimental Deformation of Pyrrhotite and Sphalerite to 2,000 Bars and 500 degrees C. Economic Geology, 68 (3) 332-352 doi:10.2113/gsecongeo.68.3.332
Barton, Paul B., Toulmin, Priestley (1964) Experimental determination of the reaction chalcopyrite+sulfur=pyrite+bornite from 350 to 500 degrees C. Economic Geology, 59 (5) 747-752 doi:10.2113/gsecongeo.59.5.747
Czamanske, Gerald K., Rye, Robert O. (1974) Experimentally Determined Sulfur Isotope Fractionations between Sphalerite and Galena in the Temperature Range 600 degrees to 275 degrees C. Economic Geology, 69 (1) 17-25 doi:10.2113/gsecongeo.69.1.17
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
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
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, 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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