THERMOCHEMISTRY OF SULFIDE MINERAL SOLUTIONS

dc.contributor.author	Sack R.O.
dc.contributor.author	Ebel D.S.
dc.date.accessioned	2025-03-15T04:58:35Z
dc.date.available	2025-03-15T04:58:35Z
dc.date.issued	2006
dc.identifier	https://elibrary.ru/item.asp?id=31323363
dc.identifier.citation	Reviews in Mineralogy and Geochemistry, 2006, 61, 61. С. 2, 265-364
dc.identifier.issn	1529-6466
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/48476
dc.description.abstract	In 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.title	THERMOCHEMISTRY OF SULFIDE MINERAL SOLUTIONS
dc.type	Статья
dc.identifier.doi	10.2138/rmg.2006.61.6

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