THERMOCHEMISTRY OF SULFIDE MINERAL SOLUTIONS

dc.contributor.authorSack R.O.
dc.contributor.authorEbel D.S.
dc.date.accessioned2025-03-15T04:58:35Z
dc.date.available2025-03-15T04:58:35Z
dc.date.issued2006
dc.description.abstractIn the sulfide mineral assemblages commonly found in terrestrial rocks, the major elements are S with the metals Fe, Zn, Cu, Pb, and Ag and semimetals As and Sb. Minor elements include Te, Se; the metals Ni, Cd, Co, Mn and the semimetals Hg and Bi. Particular ore deposits can be characterized using specific subsystems containing these elements (e.g., McKinstry 1963). Previous reviews have summarized in detail the phase relations in binary, ternary, and higher-order systems. These include Barton (1970), the first volume in this series (Craig and Scott 1976), excellent chapters by Barton and Skinner...
dc.identifierhttps://elibrary.ru/item.asp?id=31323363
dc.identifier.citationReviews in Mineralogy and Geochemistry, 2006, 61, 61. С. 2, 265-364
dc.identifier.doi10.2138/rmg.2006.61.6
dc.identifier.issn1529-6466
dc.identifier.urihttps://repository.geologyscience.ru/handle/123456789/48476
dc.titleTHERMOCHEMISTRY OF SULFIDE MINERAL SOLUTIONS
dc.typeСтатья

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