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GEOREF RECORD

The system Cu-Fe-Se; reconnaissance phase relations between 500 and 700 degrees C

Gian Piero Bernardini, Giuseppe Mazzetti and Renza Trosti-Ferroni
The system Cu-Fe-Se; reconnaissance phase relations between 500 and 700 degrees C
The Canadian Mineralogist (August 1981) 19, Part 3: 451-460

Abstract

Phase relations in the system Cu-Fe-Se at 500 degrees C have been studied in silica tubes by quenching experiments whereas the assemblages up to 700 degrees C have been established mainly through DTA runs on presynthesized charges. Synthetic eskebornite reacts on heating to form Se-intermediate solid solution and (Cu,Fe)Se (sub 2-x) , followed by Se-poor solid solution which decomposes into Cu (sub 2-x) Se and gamma -Fe (sub 1-x) Se between 635 and 640 degrees C. Synthetic (Cu,Fe)Se (sub 2-x) on heating shows an endothermic effect at 410 degrees C, a progressive loss of Se between 575 degrees and 655 degrees C and melts to a liquid of similar composition at 660 degrees C. According to the thermal behaviour of the two ternary solid solutions, the variation of phase relations between 500 degrees and 700 degrees C and consistent four-phase equilibria reactions are reported.


ISSN: 0008-4476
EISSN: 1499-1276
Coden: CAMIA6
Serial Title: The Canadian Mineralogist
Serial Volume: 19, Part 3
Title: The system Cu-Fe-Se; reconnaissance phase relations between 500 and 700 degrees C
Affiliation: Univ. Firenze, C.N.R. Ist. Mineral., Petrogr. e Geochim., Florence, Italy
Pages: 451-460
Published: 198108
Text Language: English
Summary Language: French
Publisher: Mineralogical Association of Canada, Ottawa, ON, Canada
References: 44
Accession Number: 1982-049205
Categories: Mineralogy of non-silicates
Document Type: Serial
Bibliographic Level: Analytic
Illustration Description: illus. incl. 3 tables
Country of Publication: Canada
Secondary Affiliation: GeoRef, Copyright 2017, American Geosciences Institute. Reference includes data from Mineralogical Abstracts, United KingdomTwickenhamUKUnited Kingdom
Update Code: 1982
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