Experimental investigation of the Ag-TI-Bi-Sb-S system
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.
Source:
Mineralogy and Petrology, 1995, 53, 4, 251-263Collections
Institution/Community
Hemijski fakultet / Faculty of ChemistryTY - JOUR AU - Gržetić, Ivan AU - Moh, G. PY - 1995 UR - https://cherry.chem.bg.ac.rs/handle/123456789/78 AB - 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. T2 - Mineralogy and Petrology T1 - Experimental investigation of the Ag-TI-Bi-Sb-S system VL - 53 IS - 4 SP - 251 EP - 263 DO - 10.1007/BF01160150 ER -
@article{ author = "Gržetić, Ivan and Moh, G.", year = "1995", 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.", journal = "Mineralogy and Petrology", title = "Experimental investigation of the Ag-TI-Bi-Sb-S system", volume = "53", number = "4", pages = "251-263", doi = "10.1007/BF01160150" }
Gržetić, I.,& Moh, G.. (1995). Experimental investigation of the Ag-TI-Bi-Sb-S system. in Mineralogy and Petrology, 53(4), 251-263. https://doi.org/10.1007/BF01160150
Gržetić I, Moh G. Experimental investigation of the Ag-TI-Bi-Sb-S system. in Mineralogy and Petrology. 1995;53(4):251-263. doi:10.1007/BF01160150 .
Gržetić, Ivan, Moh, G., "Experimental investigation of the Ag-TI-Bi-Sb-S system" in Mineralogy and Petrology, 53, no. 4 (1995):251-263, https://doi.org/10.1007/BF01160150 . .