gtcrustГеодинамика и тектонофизикаGeodynamics & Tectonophysics2078-502XInstitute of the Earth's crust of the Russian Academy of Sciences, Siberian Branch10.5800/GT-2024-15-3-0756PAHHPAgtcrust-1845Research ArticleПАЛЕОГЕОДИНАМИКАPALEOGEODYNAMICSГЕОДИНАМИКА И РУДОНОСНОСТЬ ПРОТЕРОЗОЙСКИХ МАФИТОВ ЦЕНТРАЛЬНОЙ ЧАСТИ АЛДАНО-СТАНОВОГО ЩИТА (ЮГ СЕВЕРО-АЗИАТСКОГО КРАТОНА)Geodynamics and Ore Content of Proterozoic Maphites in the Central Part of the Aldan-Stanovoy Shield (Southern North Asian Craton)КравченкоА. А.KravchenkoA. A.

677007, Якутск, пр-т Ленина, 39, Республика Саха (Якутия)

Alexander A. Kravchenko

39 Lenin Ave, Yakutsk 677007, Republic of Sakha (Yakutia)

kravchenkoaa@diamond.ysn.ruОкругинА. В.OkruginA. V.

677007, Якутск, пр-т Ленина, 39, Республика Саха (Якутия)

39 Lenin Ave, Yakutsk 677007, Republic of Sakha (Yakutia)

БерёзкинВ. И.BeryozkinV. I.

677007, Якутск, пр-т Ленина, 39, Республика Саха (Якутия)

39 Lenin Ave, Yakutsk 677007, Republic of Sakha (Yakutia)

ПоповН. В.PopovN. V.

630090, Новосибирск, пр-т Академика Коптюга, 3

3 Academician Koptyug Ave, Novosibirsk 630090

ЛоскутовЕ. Е.LoskutovE. E.

677007, Якутск, пр-т Ленина, 39, Республика Саха (Якутия)

39 Lenin Ave, Yakutsk 677007, Republic of Sakha (Yakutia)

Институт геологии алмаза и благородных металлов СО РАНРоссияDiamond and Precious Metal Geology Institute, Siberian Branch of the Russian Academy of SciencesRussian FederationИнститут нефтегазовой геологии и геофизики им. А.А. Трофимука СО РАНРоссияTrofimuk Institute of Petroleum Geology and Geophysics, Siberian Branch of the Russian Academy of SciencesRussian Federation202417062024153756756Copyright © Кравченко А.А., Округин А.В., Берёзкин В.И., Попов Н.В., Лоскутов Е.Е., 20242024Кравченко А.А., Округин А.В., Берёзкин В.И., Попов Н.В., Лоскутов Е.Е.Kravchenko A.A., Okrugin A.V., Beryozkin V.I., Popov N.V., Loskutov E.E.Данная работа распространяется под лицензией Creative Commons Attribution 4.0.This work is licensed under a Creative Commons Attribution 4.0 License.https://www.gt-crust.ru/jour/article/view/1845

Изучение составов мантийных магматических комплексов важно для расшифровки геодинамических событий, механизмов формирования рудных месторождений и источников рудообразующих веществ. Современные исследования орогенных месторождений золота в метаморфизованных докембрийских террейнах подтверждают важность обогащенной субдукцией литосферной мантии в процессах рудообразования. На территории Нимнырского террейна Алдано-Станового щита орогенная золотая минерализация приурочена к выходам мафических гранулитов медведевского комплекса, внедрившегося и метаморфизованного 1.92–1.90 млрд лет назад на заключительной стадии коллизионного процесса. Медведевский комплекс и рудные тела пересечены неметаморфизованными долеритами Тимптоно-гынымского и Тимптоно-алгамайского дайковых поясов с возрастом 1.87 и 1.75 млрд лет, образованными в условиях постколлизионного и внутриконтинентального растяжения. Наличие мантийных магматических комплексов различных геодинамических обстановок и этапов формирования дает возможность определить особенности состава и эволюции мантии в связи с процессами рудообразования. Для этого были определены содержания породообразующих окислов и элементов-примесей в дорудных мафических гранулитах медведевского комплекса и пострудных долеритах. На основе геохимических данных проведена реконструкция условий формирования пород и типов мантийных источников. Обнаружено, что породы медведевского комплекса образованы за счет плюмового источника. В формировании расплавов для долеритов принимал участие обогащенный процессом субдукции материал литосферной мантии. Вероятны различные степени плавления в источниках и взаимодействие плюма с обогащенной литосферной мантией на заключительной стадии коллизионного процесса. Полученные результаты могут быть использованы для уточнения геодинамических моделей формирования золоторудной минерализации в центральной части Алдано-Станового щита. Предложена одна из общепринятых моделей.

The study of diverse mantle-derived igneous complexes is important for interpreting geodynamic events, ore deposits formation mechanisms, and ore-forming fluid sources. Modern studies of orogenic gold deposits in the Precambrian metamorphosed terranes emphasize the importance of subduction-enriched lithospheric mantle in the ore formation processes. Orogenic gold mineralization in the Nimnyr terrane of the Aldan-Stanovoy shield is confined to the outcrops of mafic granulites from the Medvedev complex, intruded and metamorphosed 1.92–1.90 Ga ago at the final stage of the collision process. The Medvedev complex and ore bodies are intersected by non-metamorphosed dolerites of the 1.87 Ga Timpton-Gynym and 1.75 Ga Timpton-Algamai dike belts formed under conditions of post-collisional and intracontinental extension. The mantle-derived igneous complexes, presenting in a variety of geodynamic settings and ore mineral formation stages, make it possible to identify compositional and evolutionary features of the mantle in connection with ore formation processes. To do this, there were determined rock-forming oxide and trace element concentrations in pre-ore mafic granulites of the Medvedev complex and post-ore dolerites. Based on the geochemical data, there was a reconstruction of rock and mantle source type formation conditions. It was found that the rocks of the Medvedev complex are plume-derived. Doleritic melt formation was contributed to by the subduction-enriched lithospheric mantle material. There is a possility of different degrees of source melting and interaction of plume with the enriched lithospheric mantle at the final stage of the collision process. The obtained results can be used to refine the geodynamic models of gold mineralization formation in the central part of the Aldan-Stanovoy shield. There has been proposed one of the standard models.

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The authors declare that there are no conflicts of interest present.