SULFUR SOURCES OF SULFIDES OF THE AK-SUG CU-AU PORPHYRY DEPOSIT, EASTERN TUVA
The paper presents the S isotopic composition of sulfides from the Ak-Sug Au-Cu-porphyry deposit hosted by Early Proterozoic magmatic rocks. The S isotopic composition of sulfides varies from +1.0 to +3.2 ‰: +2.5 to +3.2 ‰ for molybdenite-I, +1.0 to +3.1 ‰ for pyrite-III, –2.3 to – 0.9 ‰ for chalcop...
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South Urals Federal Research Center of Mineralogy and Geoecology UB RAS
2019-12-01
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| Series: | Минералогия |
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| Online Access: | https://journal.mineralogy.ru/wp-content/uploads/2020/01/2019-4-6.pdf |
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| author | R.V. Kuzhuget A.O. Mongush N.N. Ankusheva |
| author_facet | R.V. Kuzhuget A.O. Mongush N.N. Ankusheva |
| author_sort | R.V. Kuzhuget |
| collection | DOAJ |
| description | The paper presents the S isotopic composition of sulfides from the Ak-Sug Au-Cu-porphyry deposit hosted by Early Proterozoic magmatic rocks. The S isotopic composition of sulfides varies from +1.0 to +3.2 ‰: +2.5 to +3.2 ‰ for molybdenite-I, +1.0 to +3.1 ‰ for pyrite-III, –2.3 to – 0.9 ‰ for chalcopyrite-III–V,–2.9 to –2.4 ‰, for chalcopyrite-VI and –1.0 ‰ for pyrite-V. The close-to-zero S isotopic ratios of sulfides from the Ak-Sug deposit indicate magmatic (from –5 to +5 ‰) or mantle (from –3 to +3 ‰) S source typical of most Cu-porphyry deposits of the Pacific Fire Ring. |
| format | Article |
| id | doaj-art-8c49e7c7152a4c4eae0cf295e7924305 |
| institution | DOAJ |
| issn | 2313-545X 2782-2044 |
| language | English |
| publishDate | 2019-12-01 |
| publisher | South Urals Federal Research Center of Mineralogy and Geoecology UB RAS |
| record_format | Article |
| series | Минералогия |
| spelling | doaj-art-8c49e7c7152a4c4eae0cf295e79243052025-08-20T02:43:15ZengSouth Urals Federal Research Center of Mineralogy and Geoecology UB RASМинералогия2313-545X2782-20442019-12-0154738210.35597/2313-545X-2019-5-4-6SULFUR SOURCES OF SULFIDES OF THE AK-SUG CU-AU PORPHYRY DEPOSIT, EASTERN TUVAR.V. Kuzhuget0A.O. Mongush1N.N. Ankusheva2Tuvinian Institute for Exploration of Natural Resources SB RASTuvinian Institute for Exploration of Natural Resources SB RASSouth Urals Federal Research Center of Mineralogy and Geoecology UB RASThe paper presents the S isotopic composition of sulfides from the Ak-Sug Au-Cu-porphyry deposit hosted by Early Proterozoic magmatic rocks. The S isotopic composition of sulfides varies from +1.0 to +3.2 ‰: +2.5 to +3.2 ‰ for molybdenite-I, +1.0 to +3.1 ‰ for pyrite-III, –2.3 to – 0.9 ‰ for chalcopyrite-III–V,–2.9 to –2.4 ‰, for chalcopyrite-VI and –1.0 ‰ for pyrite-V. The close-to-zero S isotopic ratios of sulfides from the Ak-Sug deposit indicate magmatic (from –5 to +5 ‰) or mantle (from –3 to +3 ‰) S source typical of most Cu-porphyry deposits of the Pacific Fire Ring.https://journal.mineralogy.ru/wp-content/uploads/2020/01/2019-4-6.pdfsulfidessulfur isotopescopper porphyry depositstuva |
| spellingShingle | R.V. Kuzhuget A.O. Mongush N.N. Ankusheva SULFUR SOURCES OF SULFIDES OF THE AK-SUG CU-AU PORPHYRY DEPOSIT, EASTERN TUVA Минералогия sulfides sulfur isotopes copper porphyry deposits tuva |
| title | SULFUR SOURCES OF SULFIDES OF THE AK-SUG CU-AU PORPHYRY DEPOSIT, EASTERN TUVA |
| title_full | SULFUR SOURCES OF SULFIDES OF THE AK-SUG CU-AU PORPHYRY DEPOSIT, EASTERN TUVA |
| title_fullStr | SULFUR SOURCES OF SULFIDES OF THE AK-SUG CU-AU PORPHYRY DEPOSIT, EASTERN TUVA |
| title_full_unstemmed | SULFUR SOURCES OF SULFIDES OF THE AK-SUG CU-AU PORPHYRY DEPOSIT, EASTERN TUVA |
| title_short | SULFUR SOURCES OF SULFIDES OF THE AK-SUG CU-AU PORPHYRY DEPOSIT, EASTERN TUVA |
| title_sort | sulfur sources of sulfides of the ak sug cu au porphyry deposit eastern tuva |
| topic | sulfides sulfur isotopes copper porphyry deposits tuva |
| url | https://journal.mineralogy.ru/wp-content/uploads/2020/01/2019-4-6.pdf |
| work_keys_str_mv | AT rvkuzhuget sulfursourcesofsulfidesoftheaksugcuauporphyrydepositeasterntuva AT aomongush sulfursourcesofsulfidesoftheaksugcuauporphyrydepositeasterntuva AT nnankusheva sulfursourcesofsulfidesoftheaksugcuauporphyrydepositeasterntuva |