Ключевые слова

2411-3336

2541-9404

Записки Горного института

Journal of Mining Institute

Санкт-Петербургский горный университет императрицы Екатерины ΙΙ

Empress Catherine II Saint Petersburg Mining University

SRITGO

pmi-16344

https://pmi.spmi.ru/pmi/article/view/16344

Геология

Geology

Paleoproterozoic Saltakh Pluton, Anabar Shield: mineralogical composition, age and a geodynamic setting

Палеопротерозойский Салтахский плутон (Анабарский щит): вещественный состав, возраст, геодинамическая обстановка формирования

Gusev

Nikolai I.

Гусев

Н. И.

Gusev

Nikolai I.

Nikolay_Gusev@vsegei.ru

0000-0002-3461-0961

Всероссийский научно-исследовательский геологический институт им. А.П.Карпинского (Санкт-Петербург, Россия) Karpinsky Russian Geological Research Institute (Saint Petersburg, Russia)

Romanova

Lyudmila Yu.

Романова

Л. Ю.

Romanova

Lyudmila Yu.

sergeeva.luda02@yandex.ru

0009-0005-2766-0097

26 08 2024

2025

272 16 39 10 11 2023 02 05 2024 25 04 2025

2024

Н. И. Гусев, Л. Ю. Романова

Nikolai I. Gusev, Lyudmila Yu. Romanova

CC BY 4.0

https://pmi.spmi.ru/pmi/article/view/16344

Салтахский массив расположен в северной части Анабарского щита в Салтахской зоне смятия. Массив сложен двупироксеновыми кристаллосланцами и плагиогнейсами гранулитовой фации метаморфизма, по химическому составу соответствующими дифференцированной серии пород от габбро до тоналитов с многочисленными жилами и телами аляскитовых гнейсогранитов. Большей частью породы калиевые (K2O/Na2O > 0,50), магнезиальные (mg# 50-70), в метагабброидах нормативный оливин составляет 6-9%, низкотитанистые (TiO2 0,35-1,31 мас. %) с низким содержанием TiO2 в клино- и ортопироксене. Породы характеризуются хорошо выраженными отрицательными аномалиями Ti, Nb, Ta, P, свойственными субдукционному магматизму. Двупироксеновые гнейсы отличаются высокими значениями Sr/Y = 67,6-88, (La/Yb)N = 24,8-25,6. По индикаторным отношениям Nb/La, La/Yb, Th/Nb, Ce/Yb породы массива относятся к шошонитовой серии. Все породы характеризуются положительными величинами εNd(T) = 1,9-4,1, εSr(T) = 0,77-17,8, указывающими на мантийный источник магмы, и величиной T(Nd)DM = 2,20-2,26 млрд лет. По данным U-Pb датирования циркона (SHRIMP II) протолиты меланократовых пород массива имеют возраст 2100-2086 млн лет, двупироксеновых плагиогнейсов тоналитового состава – 2025±7 млн лет. Возраст аляскитовых гнейсогранитов 1969±7 млн лет. Изучение редкоэлементного состава циркона показало повсеместную обогащенность LREE. Причинами высокого содержания LREE являются как вторичные изменения циркона, так и шошонитовый характер расплава, высокотемпературные условия кристаллизации и аномальный флюидный режим. Геодинамическая обстановка формирования Салтахского массива соответствовала периконтинентальной магматической дуге. Формирование аляскитовых гнейсогранитов является следствием анатексиса в связи с более поздними коллизионными процессами. Магматические породы Салтахского массива по возрасту синхронны расположенным южнее ранее изученным магматическим образованиям Хапчанского участка (толеитовые метадиориты 2095±10 млн лет, известково-щелочные метатоналиты 2030±17 млн лет) и интерпретируются нами как часть метаморфизованного ювенильного палеопротерозойского надсубдукционного комплекса.

The Saltakh Massif is located in the northern Anabar Shield, in the Saltakh shear-zone. It consists of two-pyroxene schists and plagiogneisses metamorphosed under granulite-facies conditions. Their chemical composition is consistent with that of a differentiated series of rocks ranging from gabbro to tonalites with abundant alaskitic gneissose granite veins and bodies. The rocks are mainly high-potassium (K2O/Na2O > 0.50), high-magnesium (mg# 50-70), low-titanium (TiO2 0.35-1.31 wt.%) with low TiO2 concentration in clino- and orthopyroxene. Normative olivine makes up 6-9 % of metagabbroic rocks. The rocks display well-defined negative Ti, Nb, Ta, and P anomalies typical of subduction magmatism. The two-pyroxene gneisses show high Sr/Y ratios of 67.6-88 and (La/Yb)N of 24.8-25.6. Saltakh rocks are part of a shoshonite series, as indicated by Nb/La, La/Yb, Th/Nb and Ce/Yb ratios. All the rocks display positive εNd(T) values of 1.9-4.1 and εSr(T) of 0.77-17.8 indicative of a mantle source of magma and T(Nd)DM of 2,20-2,26 Ga. U-Pb zircon dating (SHRIMP II) has shown that the protoliths of Saltakh melanocratic rocks were dated at 2100-2086 Ma, and those of two-pyroxene plagiogneisses of tonalite composition were dated at 2025±7 Ma. Alaskitic gneissose granites were dated at 1969±7 Ma. The study of the trace element composition of zircon has revealed general enrichment in LREE. High LREE concentrations are due to secondary zircon alterations and the shoshonitic pattern of the melt, the high-temperature conditions of crystallization, and an anomalous fluid regime. The geodynamic setting in which the Saltakh Massif was formed was consistent with a pericontinental magmatic arc. The formation of alaskitic gneissose granites was due to anatexis provoked by later collision processes. Saltakh magmatic rocks were formed simultaneously with magmatic rocks from the Khapchan prospect which occur farther south, and were studied earlier (2095±10 Ma tholeiitic metadiorites and 2030±17 Ma calc-alkaline metatonalites). We interpret them as part of a metamorphosed juvenile Paleoproterozoic suprasubduction complex.

Ключевые слова Анабарский щит Салтахский массив гранулиты U-Pb метод геохронология

Keywords Anabar Shield Saltakh Massif granulites U-Pb method geochronology

Исследования выполнены в рамках проекта Российского научного фонда № 23-27-00098.

Studies were conducted under Russian Science Foundation project N 23-27-00098.

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