Ge-Hg-Rich Sphalerite and Pb, Sb, As, Hg, and Ag Sulfide Assemblages in Mud Volcanoes of Sakhalin Island, Russia: An Insight into Possible Origin

We characterize the mineralogy and geochemistry of Fe, Zn, Pb, Sb, As, Hg, Ag sulfide assemblages from mud masses currently extruded by the onshore South Sakhalin and Pugachev mud volcanoes (Sakhalin Island, Russia). Abundant Tl-rich pyrite in sulfide concentrate samples from the mud volcanoes coexi...

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Autores principales: Ella V. Sokol, Svetlana N. Kokh, Anna V. Nekipelova, Adam Abersteiner, Yurii V. Seryotkin, Valeriy V. Ershov, Olga A. Nikitenko, Anna S. Deviatiiarova
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Publicado: MDPI AG 2021
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spelling oai:doaj.org-article:4cc86dae6344448eabe4de8ed3aa00e22021-11-25T18:26:04ZGe-Hg-Rich Sphalerite and Pb, Sb, As, Hg, and Ag Sulfide Assemblages in Mud Volcanoes of Sakhalin Island, Russia: An Insight into Possible Origin10.3390/min111111862075-163Xhttps://doaj.org/article/4cc86dae6344448eabe4de8ed3aa00e22021-10-01T00:00:00Zhttps://www.mdpi.com/2075-163X/11/11/1186https://doaj.org/toc/2075-163XWe characterize the mineralogy and geochemistry of Fe, Zn, Pb, Sb, As, Hg, Ag sulfide assemblages from mud masses currently extruded by the onshore South Sakhalin and Pugachev mud volcanoes (Sakhalin Island, Russia). Abundant Tl-rich pyrite in sulfide concentrate samples from the mud volcanoes coexists with common Hg- and Ge-rich sphalerite, as well as with sporadic boulangerite, robinsonite, bournonite, galena, realgar, metacinnabar, cinnabar, acanthite, and chalcopyrite. Sphalerites are remarkably enriched in Hg (locally reaching 27 wt%) and coupled zwith permanent abnormal enrichment in Ge (3008–3408 ppm). According to single-crystal XRD analyses and Raman spectroscopy, both Hg-poor and Hg-rich sphalerites are single-phase (Zn,Hg)S<sub>cub</sub> compounds. Pyrite is of diagenetic origin, judging by its trace-element chemistry, particular morphology, and heavy S isotope composition. Another assemblage, composed of Pb-Sb-(Hg) sulfide minerals and lesser As, Cu, Ag, and Bi compounds, results from hydrothermal alteration and is genetically related to Neogene volcano-sedimentary rocks found among the ejecta of the mud volcanoes. The composition of impurities in sphalerite from mud masses indicates crystallization at temperatures lower than ~100 °C, under the leaching effect of mud volcano waters.Ella V. SokolSvetlana N. KokhAnna V. NekipelovaAdam AbersteinerYurii V. SeryotkinValeriy V. ErshovOlga A. NikitenkoAnna S. DeviatiiarovaMDPI AGarticlesphaleritemetacinnabarcinnabarZnS-HgS seriesPb-Sb sulfosaltsLA-ICPMSMineralogyQE351-399.2ENMinerals, Vol 11, Iss 1186, p 1186 (2021)
institution DOAJ
collection DOAJ
language EN
topic sphalerite
metacinnabar
cinnabar
ZnS-HgS series
Pb-Sb sulfosalts
LA-ICPMS
Mineralogy
QE351-399.2
spellingShingle sphalerite
metacinnabar
cinnabar
ZnS-HgS series
Pb-Sb sulfosalts
LA-ICPMS
Mineralogy
QE351-399.2
Ella V. Sokol
Svetlana N. Kokh
Anna V. Nekipelova
Adam Abersteiner
Yurii V. Seryotkin
Valeriy V. Ershov
Olga A. Nikitenko
Anna S. Deviatiiarova
Ge-Hg-Rich Sphalerite and Pb, Sb, As, Hg, and Ag Sulfide Assemblages in Mud Volcanoes of Sakhalin Island, Russia: An Insight into Possible Origin
description We characterize the mineralogy and geochemistry of Fe, Zn, Pb, Sb, As, Hg, Ag sulfide assemblages from mud masses currently extruded by the onshore South Sakhalin and Pugachev mud volcanoes (Sakhalin Island, Russia). Abundant Tl-rich pyrite in sulfide concentrate samples from the mud volcanoes coexists with common Hg- and Ge-rich sphalerite, as well as with sporadic boulangerite, robinsonite, bournonite, galena, realgar, metacinnabar, cinnabar, acanthite, and chalcopyrite. Sphalerites are remarkably enriched in Hg (locally reaching 27 wt%) and coupled zwith permanent abnormal enrichment in Ge (3008–3408 ppm). According to single-crystal XRD analyses and Raman spectroscopy, both Hg-poor and Hg-rich sphalerites are single-phase (Zn,Hg)S<sub>cub</sub> compounds. Pyrite is of diagenetic origin, judging by its trace-element chemistry, particular morphology, and heavy S isotope composition. Another assemblage, composed of Pb-Sb-(Hg) sulfide minerals and lesser As, Cu, Ag, and Bi compounds, results from hydrothermal alteration and is genetically related to Neogene volcano-sedimentary rocks found among the ejecta of the mud volcanoes. The composition of impurities in sphalerite from mud masses indicates crystallization at temperatures lower than ~100 °C, under the leaching effect of mud volcano waters.
format article
author Ella V. Sokol
Svetlana N. Kokh
Anna V. Nekipelova
Adam Abersteiner
Yurii V. Seryotkin
Valeriy V. Ershov
Olga A. Nikitenko
Anna S. Deviatiiarova
author_facet Ella V. Sokol
Svetlana N. Kokh
Anna V. Nekipelova
Adam Abersteiner
Yurii V. Seryotkin
Valeriy V. Ershov
Olga A. Nikitenko
Anna S. Deviatiiarova
author_sort Ella V. Sokol
title Ge-Hg-Rich Sphalerite and Pb, Sb, As, Hg, and Ag Sulfide Assemblages in Mud Volcanoes of Sakhalin Island, Russia: An Insight into Possible Origin
title_short Ge-Hg-Rich Sphalerite and Pb, Sb, As, Hg, and Ag Sulfide Assemblages in Mud Volcanoes of Sakhalin Island, Russia: An Insight into Possible Origin
title_full Ge-Hg-Rich Sphalerite and Pb, Sb, As, Hg, and Ag Sulfide Assemblages in Mud Volcanoes of Sakhalin Island, Russia: An Insight into Possible Origin
title_fullStr Ge-Hg-Rich Sphalerite and Pb, Sb, As, Hg, and Ag Sulfide Assemblages in Mud Volcanoes of Sakhalin Island, Russia: An Insight into Possible Origin
title_full_unstemmed Ge-Hg-Rich Sphalerite and Pb, Sb, As, Hg, and Ag Sulfide Assemblages in Mud Volcanoes of Sakhalin Island, Russia: An Insight into Possible Origin
title_sort ge-hg-rich sphalerite and pb, sb, as, hg, and ag sulfide assemblages in mud volcanoes of sakhalin island, russia: an insight into possible origin
publisher MDPI AG
publishDate 2021
url https://doaj.org/article/4cc86dae6344448eabe4de8ed3aa00e2
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