1987
DOI: 10.1007/bf01163259
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Mutual Pb2+/Sn2+ substitution in sulfosalts

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Cited by 9 publications
(6 citation statements)
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“…To probe the stoichiometry analysis, we employed energy-dispersive X-ray spectroscopy technique that results in an approximate chemical formula Pb6Sn3Sb3FeS18 (see the Supplementary Information), which falls within the generic chemical formula (Pb, Sn) 6+x 2+ Sb 2 3+ Fe 2+ Sn 2 4+ S 14+x , where −1 ≤ 𝑥 ≤ 0.25 of materials from a mine in Bolivia. 6 This confirms the origin of our samples which are originated from a mine in San Jose, Bolivia.…”
supporting
confidence: 80%
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“…To probe the stoichiometry analysis, we employed energy-dispersive X-ray spectroscopy technique that results in an approximate chemical formula Pb6Sn3Sb3FeS18 (see the Supplementary Information), which falls within the generic chemical formula (Pb, Sn) 6+x 2+ Sb 2 3+ Fe 2+ Sn 2 4+ S 14+x , where −1 ≤ 𝑥 ≤ 0.25 of materials from a mine in Bolivia. 6 This confirms the origin of our samples which are originated from a mine in San Jose, Bolivia.…”
supporting
confidence: 80%
“…To probe the stoichiometry analysis, we employed the energy-dispersive X-ray (EDX) spectroscopy technique, which results in an approximate chemical formula of Pb S 14+x , where −1 ≤ x ≤ 0.25, of materials from a mine in Bolivia. 8,9 This confirms the origin of our samples, which originate from a mine in San Jose, Bolivia.…”
supporting
confidence: 80%
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“…The mutual Pb 2+ / Sn 2+ substitution in the structure of sul des and sulfosalts is well known (Moh, 1987), and this series is a typical example. Natural occurrences of herzenbergite-teallite minerals have been reported from several localities (Nekrasov et al, 1974;Berndt, 1954;Hayashi, 1986, Smeds, 1993), the most important of these being the Bolivian polymetallic ores.…”
Section: Introductionmentioning
confidence: 97%
“…Sn 4+ 2S14+x, with -1 ≤ x ≤ 0.25 21 . Franckeite constitutes a natural misfit compound mineral, whose superlattice structure has been formed by alternating phase segregation of pseudo-hexagonal Sn-rich and pseudo-tetragonal Pb-rich layers, separated by a van der Waals gap (Figure 1(a)).…”
Section: Introductionmentioning
confidence: 99%