Abstract
Phase relations were determined in the Cu-Te-S system at 350, 450,
550, 675, 800 and 900 degree C. At 350 degree C three ternary
phases are present, goldfieldite and two phases A and B, which
have not been found i nature. Phase A has disappeared by 450
degree C, goldfieldite has disappeared by 550 degree C, and phase
B has disappeared by 800 degree C. Godlfieldite and phase A
(Cu5Te4S8) have no detectable compositional ranges. Goldfieldidte
has a cubic, face centered cell with a=10.242(22) Å. Phase A is
monoclinic primitive, a = 6.51 Å, b = 3.72 Å, c = 18.11 Å, beta =
80.84 degree and Z = 1. Phase B has a long and narrow
compositional field at all temperature levels with nearly constant
Cu content and an ideal formula based on 16 atoms is Cu10(Te6-xSx)
with 0.4>x>3.3 and Z = 10. The phase is cubic body
centeret with a ranging from 14.337(103) Å (S-poor) to 14.827(69)
Å (S-rich). X-ray powder data and optical data on phases A and B
are listed. At 350 degree C there exist two liquid fields which at
450 degree C have become one continuous field stretching from
Cu45Te55 with low S content to the tellurium corner of the phase
diagram and from there to the sulphur corner. With increasing S,
the Cu content of the liquid rapidly decreases to trace amonts.
With increasing temperature the field extends into the ternary
from the tellurium corner towards the Cu-S join. The boundary of
the liquid field in the central portion of the phae diagram
towards the sulphur corner does not change position with an
increase in temperature from 550 to 900 degree C.
Original language | English |
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Journal | N.Jb.Miner.Abh. |
Volume | 166 |
Issue number | 2 |
Pages (from-to) | 113 to 136 |
Publication status | Published - 1994 |