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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

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Reference TypeJournal (article/letter/editorial)
TitleSolubility 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
JournalEconomic Geology
AuthorsWood, Scott A.Author
Crerar, David A.Author
Borcsik, Maria P.Author
Year1987 (November 1)Volume82
Issue7
PublisherSociety of Economic Geologists
DOIdoi:10.2113/gsecongeo.82.7.1864Search in ResearchGate
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Mindat Ref. ID228745Long-form Identifiermindat:1:5:228745:8
GUID0
Full ReferenceWood, 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
Plain TextWood, 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
In(1987, November) Economic Geology Vol. 82 (7) Society of Economic Geologists

See Also

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Crerar, David A., Susak, N.J., Borcsik, M., Schwartz, S. (1978) Solubility of the buffer assemblage pyrite + pyrrhotite + magnetite in NaCl solutions from 200 to 350°C. Geochimica et Cosmochimica Acta, 42 (9) 1427-1437 doi:10.1016/0016-7037(78)90048-0
Wood, Scott A., Mountain, Bruce W. (1991) Hydrothermal solubility of palladium in chloride solutions from 300 degrees to 700 degrees C; preliminary experimental results; discussion. Economic Geology, 86 (7) 1562-1563 doi:10.2113/gsecongeo.86.7.1562
Crerar, D. A., Barnes, H. L. (1976) Ore solution chemistry; V, Solubilities of chalcopyrite and chalcocite assemblages in hydrothermal solution at 200 degrees to 350 degrees C. Economic Geology, 71 (4) 772-794 doi:10.2113/gsecongeo.71.4.772
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
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
Hsu, L. C., Lechler, Paul J., Nelson, John H. (1991) Hydrothermal solubility of palladium in chloride solutions from 300 degrees to 700 degrees C; preliminary experimental results. Economic Geology, 86 (2) 422-427 doi:10.2113/gsecongeo.86.2.422
Anderson, G. M. (1973) The Hydrothermal Transport and Deposition of Galena and Sphalerite Near 100 degrees C. Economic Geology, 68 (4) 480-492 doi:10.2113/gsecongeo.68.4.480
Giordano, T. H., Barnes, H. L. (1979) Ore solution chemistry VI; PbS solubility in bisulfide solutions to 300 degrees C. Economic Geology, 74 (7) 1637-1646 doi:10.2113/gsecongeo.74.7.1637
Bourcier, W. L., Barnes, H. L. (1987) Ore solution chemistry; VII, Stabilities of chloride and bisulfide complexes of zinc to 350 degrees C. Economic Geology, 82 (7) 1839-1863 doi:10.2113/gsecongeo.82.7.1839
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
Posey-Dowty, J., Axtmann, E., Crerar, David A., Borcsik, Maria P., Ronk, A., Woods, W. (1987) Dissolution rate of uraninite and uranium roll-front ores. Economic Geology, 82 (1) 184-194 doi:10.2113/gsecongeo.82.1.184
 
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