Study was given to a fragment of the phase diagram of the system Fe–FeS–NiS–Ni at 900 °C in the field of the monosulfide solid solution (mss) + sulfide melt (L) equilibrium and in its vicinity. The samples after isothermal annealing and quenching were studied by microscopy and X-ray diffraction and electron microprobe analyses. Tie lines in the L + mss field and the position of the boundary of this field have been determined. Also, the sides of the triangle L + mss + taenite has been refined, and the dependences of the mss–melt partition coefficients of all components on the melt composition have been established. Using the pyrrhotite method, sulfur fugacity fS2 was measured along the sections with 51, 48, and 45 at.% S and the FeS–Ni3S2 section at 900 °C.
Skip Nav Destination
Article navigation
Research Article|
July 01, 2006
PHASE RELATIONSHIPS AND SULFUR FUGACITY IN THE SYSTEM Fe–FeS–NiS–Ni AT 900°C
E.F. Sinyakova;
E.F. Sinyakova
Institute of Geology and Mineralogy, Siberian Branch of the RAS, 3 prosp. Akad. Koptyuga, Novosibirsk, 630090, Russia
Search for other works by this author on:
V.I. Kosyakov
V.I. Kosyakov
*
Nikolaev Institute of Inorganic Chemistry, Siberian Branch of the RAS, 3 prosp. Akad. Lavrent’eva, Novosibirsk, 630090, Russia
Search for other works by this author on:
E.F. Sinyakova
Institute of Geology and Mineralogy, Siberian Branch of the RAS, 3 prosp. Akad. Koptyuga, Novosibirsk, 630090, Russia
V.I. Kosyakov
*
Nikolaev Institute of Inorganic Chemistry, Siberian Branch of the RAS, 3 prosp. Akad. Lavrent’eva, Novosibirsk, 630090, Russia
Publisher: Novovsibirsk State University
Received:
04 Apr 2005
First Online:
29 Oct 2022
Online ISSN: 1878-030X
Print ISSN: 1068-7971
© 2006 UIGGM, SIBERIAN BRANCH OF THE RAS
UIGGM, SIBERIAN BRANCH OF THE RAS
Russ. Geol. Geophys. (2006) 47 (7): 838–849.
Article history
Received:
04 Apr 2005
First Online:
29 Oct 2022
Citation
E.F. Sinyakova, V.I. Kosyakov; PHASE RELATIONSHIPS AND SULFUR FUGACITY IN THE SYSTEM Fe–FeS–NiS–Ni AT 900°C. Russ. Geol. Geophys. 2006;; 47 (7): 838–849. doi:
Download citation file:
You could not be signed in. Please check your email address / username and password and try again.
Email alerts
Index Terms/Descriptors
Citing articles via
Related Articles
BEHAVIOR OF PGE ON CRYSTALLIZATION OF MELTS OF THE SYSTEM Fe–Ni–S (Fe x Ni 0.49– x S 0.51 SECTION)
Russian Geology and Geophysics
COLLECTORS OF Pt, Pd AND Rh IN A S-POOR Fe–Ni–Cu SULFIDE SYSTEM AT 760°C: EXPERIMENTAL DATA AND APPLICATION TO ORE DEPOSITS
The Canadian Mineralogist
FORMS OF PALLADIUM RELEASE UNDER CRYSTALLIZATION OF SULFIDE MELTS OF THE Fe–Ni–S SYSTEM AT SULFUR CONTENT 40–51 AT. %
Russian Geology and Geophysics
Related Book Content
Theoretical constraints on the chemistry of the magmatic aqueous phase
Ore-bearing Granite Systems; Petrogenesis and Mineralizing Processes
Serpentinization-related nickel, iron, and cobalt sulfide, arsenide, and intermetallic minerals in an unusual inland tectonic setting, southern Arizona, USA
Tectonics, Sedimentary Basins, and Provenance: A Celebration of the Career of William R. Dickinson
Internal differentiation of rare-element pegmatites; A synthesis of recent research
Ore-bearing Granite Systems; Petrogenesis and Mineralizing Processes
Controls on ore metal ratios in granite-related ore systems: an experimental and computational approach
The Second Hutton Symposium on the Origin of Granites and Related Rocks