Vanin, V.A., Chugaev, A.V., Demonterova, E.I., Gladkochub, D.P., Mazukabzov, A.M. (2018) Geologic structure of the Mukodek gold field (northern Transbaikalia) and sources of matter (Pb-Pb and Sm-Nd data). Russian Geology and Geophysics, 59 (9). 1078-1086 doi:10.1016/j.rgg.2018.08.002
| Reference Type | Journal (article/letter/editorial) | ||
|---|---|---|---|
| Title | Geologic structure of the Mukodek gold field (northern Transbaikalia) and sources of matter (Pb-Pb and Sm-Nd data) | ||
| Journal | Russian Geology and Geophysics | ||
| Authors | Vanin, V.A. | Author | |
| Chugaev, A.V. | Author | ||
| Demonterova, E.I. | Author | ||
| Gladkochub, D.P. | Author | ||
| Mazukabzov, A.M. | Author | ||
| Vanin, V.A. | Author | ||
| Chugaev, A.V. | Author | ||
| Demonterova, E.I. | Author | ||
| Gladkochub, D.P. | Author | ||
| Mazukabzov, A.M. | Author | ||
| Year | 2018 (September) | Volume | 59 |
| Page(s) | 1078-1086 | Issue | 9 |
| Publisher | Publishing House SB RAS | ||
| DOI | doi:10.1016/j.rgg.2018.08.002Search in ResearchGate | ||
| Generate Citation Formats | |||
| Classification | Not set | LoC | Not set |
| Mindat Ref. ID | 243119 | Long-form Identifier | mindat:1:5:243119:6 |
| GUID | 0 | ||
| Full Reference | Vanin, V.A., Chugaev, A.V., Demonterova, E.I., Gladkochub, D.P., Mazukabzov, A.M. (2018) Geologic structure of the Mukodek gold field (northern Transbaikalia) and sources of matter (Pb-Pb and Sm-Nd data). Russian Geology and Geophysics, 59 (9). 1078-1086 doi:10.1016/j.rgg.2018.08.002 | ||
| Plain Text | Vanin, V.A., Chugaev, A.V., Demonterova, E.I., Gladkochub, D.P., Mazukabzov, A.M. (2018) Geologic structure of the Mukodek gold field (northern Transbaikalia) and sources of matter (Pb-Pb and Sm-Nd data). Russian Geology and Geophysics, 59 (9). 1078-1086 doi:10.1016/j.rgg.2018.08.002 | ||
| In | (2018, September) Russian Geology and Geophysics Vol. 59 (9) Publishing House SB RAS | ||
| Abstract/Notes | The Mukodek gold field is located in the Yana zone of the Baikal–Muya fold belt (northern Transbaikalia). Its orebodies are gold-bearing metasomatites confined to the fault of NE strike. It is shown that pre-ore faults played a crucial role in the spatial localization of the orebodies, as they favored the concentration of ore-bearing fluids. Results of geological and structural studies, along with available geochronological data (40Ar–39Ar dates for micas in gold-bearing pyrite), testify to ore-forming processes in the ore field during two Late Paleozoic stages. Early gold-bearing metasomatites of sericite–chlorite–albite–ankerite–quartz composition formed at 320 Ma, and late gold-bearing vein metasomatites of ankerite(calcite)–quartz composition originated at 285 Ma. A Pb–Pb isotope study of gold mineralization has shown that ore lead was supplied into the mineral-forming system mainly from a mantle source, most likely, regional Neoproterozoic igneous rocks. According to Sm–Nd isotope data, these rocks formed with the participation of a material of mantle genesis. | ||
Map of Localities
Locality Pages
| Locality | Citation Details |
|---|---|
| Mukodek ore field, Okinsky District, Buryatia, Russia |
See Also
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