Experimental investigation of the Ag-TI-Bi-Sb-S system

dc.creator	Gržetić, Ivan
dc.creator	Moh, G.
dc.date.accessioned	2018-11-22T00:00:51Z
dc.date.available	2018-11-22T00:00:51Z
dc.date.issued	1995
dc.identifier.issn	0930-0708
dc.identifier.uri	https://cherry.chem.bg.ac.rs/handle/123456789/78
dc.description.abstract	Polymetallic ore deposits of low temperature origin often contain thallium as a minor element. By means of modern analytical methods numerous new T1 minerals are described, but their coexistence and equilibria are not investigated yet. The equilibria at 200°C of the quasi-quaternary system Ag2S-Tl2S-Sb2-Sb2S3-Bi2S3 and the corresponding subsystems were studied. The system Ag2S-Tl2S-Sb2S3-Bi2S3 contains only one quasiquaternary phase, AgTlSbBiS4, which is connected by tie-lines with all quasiternary phases in the system (Ag4Sb3BiS8 and Ag3Tl3Sb2S6) and with most quasibinary phases: SbBiS3, weissbergite (TlSbS2), (TlBiS2, pyrargyrite (Ag3SbS3), miargyrite (AgSbS2) and matildite (AgBiS2). This phase diagram makes it possible to investigate all important naturally occurring parageneses of Ag and Tl sulphosalts containing Sb and Bi. © 1995 Springer-Verlag.	en
dc.rights	restrictedAccess
dc.source	Mineralogy and Petrology
dc.title	Experimental investigation of the Ag-TI-Bi-Sb-S system	en
dc.type	article
dc.rights.license	ARR
dc.citation.volume	53
dc.citation.issue	4
dc.citation.spage	251
dc.citation.epage	263
dc.identifier.doi	10.1007/BF01160150
dc.citation.other	53(4): 251-263
dc.type.version	publishedVersion	en
dc.identifier.scopus	2-s2.0-34249761887

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