gtcrustГеодинамика и тектонофизикаGeodynamics & Tectonophysics2078-502XInstitute of the Earth's crust of the Russian Academy of Sciences, Siberian Branch10.5800/GT-2024-15-6-0796BGGUPKgtcrust-1944Research ArticleПАЛЕОГЕОДИНАМИКАPALEOGEODYNAMICSВЕЩЕСТВЕННЫЙ СОСТАВ, ВОЗРАСТ И МЕТАЛЛОГЕНИЧЕСКИЙ ПОТЕНЦИАЛ ГРАНИТОИДОВ ХОТУГУ-ЭЕКИТСКОГО МАССИВА И ДАЙКИ РИОЛИТОВ СОЛОЛИЙСКОГО ПОДНЯТИЯMATERIAL COMPOSITION, ISOTOPIC-GEOCHRONOLOGICAL STUDIES AND METALLOGENIC POTENTIAL OF GRANITES OF THE KHOTUGU-EYEKIT MASSIF AND RHYOLITE DIKE OF THE SOLOLI UPLIFTИвановА. И.IvanovA. I.

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

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

ГерасимовБ. Б.GerasimovB. B.

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

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

ИвановМ. С.IvanovM. S.

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

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

ЖуравлевА. И.ZhuravlevA. I.

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

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

ВасильевД. А.VasilievD. A.

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

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

КондратьевА. И.KondratievA. I.

677000, Якутск, ул. Кирова, 18Б, Республика Саха (Якутия)

18B, Kirov St, Yakutsk, 677000, 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 FederationАО «Алмазы Анабара»РоссияJSC “Almazy Anabara”Russian Federation202413122024156796796Copyright © Иванов А.И., Герасимов Б.Б., Иванов М.С., Журавлев А.И., Васильев Д.А., Кондратьев А.И., 20242024Иванов А.И., Герасимов Б.Б., Иванов М.С., Журавлев А.И., Васильев Д.А., Кондратьев А.И.Ivanov A.I., Gerasimov B.B., Ivanov M.S., Zhuravlev A.I., Vasiliev D.A., Kondratiev A.I.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/1944

В работе дано описание петрографического и петрогеохимического состава гранитоидов Хотугу-Эекитского массива и дайки риолитов Сололийского поднятия. Выявлено, что породы массива представлены микроклиновыми гранитами. Массив монотонен по своему составу, т.е. без видимых фациальных переходов и разностей фаз внедрения. Помимо пород массива, на рассматриваемой территории развиты малые тела даек риолитов, породы которых сильно изменены вторичными процессами. Выдвинуто предположение о догранитоидном происхождении этих даек и об их интенсивной постмагматической проработке. На основе содержания основных петроокислов, значений их отношений и соотношений, а также индикаторных петрохимических коэффициентов сделан вывод о том, что породы Хотугу-Эекитского массива наиболее близки к плюмазитовым гранитам A2-типа высококалиевой известково-щелочной петрохимической серии. Основные геохимические критерии свидетельствуют о двойственной природе гранитов Хотугу-Эекитского массива, имеющих близость к гранитоидам коллизионной обстановки формирования территории, а их петрогенезис связан, по всей видимости, как со смешанным корово-мантийным, так и с чисто коровым источником. По тем же параметрам составов установлена принадлежность дайки риолитов к низкощелочным образованиям толеитовой серии, отвечающим таковым плюмазитового редкометалльного ряда коровой природы. На основе U-Pb датирования установлен абсолютный возраст даек риолитов – 2146±13 млн лет, по тому же методу и геологическим данным выдвинуто предположение о мезозойском возрасте Хотугу-Эекитского массива 186.7–157.2 млн лет. Анализ минерагенической специализации Хотугу-Эекитского массива и дайки риолитов, выполненный на основе геохимических данных, позволяет отнести изученные образования к продуктивным в отношении золотоносного рудообразования.

The paper describes the petrographic and petro-geochemical composition of granitoids of the Khotugu-Eyekit massif and the rhyolite dike of the Sololi uplift. It was revealed that the rocks of the massif are represented by microcline granites. The massif is monotonous in composition, i.e. it does not exhibit any facies transitions or differences in intrusion phases. In addition to the massif rocks, the study area is characterized by a widespread occurrence of small bodies of rhyolite dike rocks that have been strongly altered by secondary processes. An assumption was made about the pre-granitoid origin of these dikes and their intensive post-magmatic alteration. Based on the content of basic petrooxides, its ratios and relationships, as well as indicator petrochemical coefficients, it was concluded that the rocks of the Khotugu-Eyekit massif are most similar to the A2-type plumasite granites of the high-potassium calc-alkaline petrochemical series. The main geochemical criteria indicate the dual nature of the granites of the Khotugu-Eyekit massif, which are similar to the granitoids of the collisional formation setting of the area, and their petrogenesis is apparently associated with both mixed crust-mantle and purely crustal source. The same compositional parameters suggest that the rhyolite dike belongs to low-alkaline formations of the tholeiitic series, corresponding to those of the plumasite rare metal series of the crustal nature. The U-Pb dating yielded an absolute age of 2146±13 Ma for the rhyolite dikes; the same method and the geological data imply that the Khotugu-Eyekit massif is Mesozoic in age, dating back to 186.7–157.2 Ma. Mineragenic specialization analysis of the Khotugu-Eyekit massif and the rhyolite dike, performed on the basis of the geochemical data, allows classifying the studied formations as productive in terms of gold-bearing ore formations.

 

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