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

QRFPEW

pmi-16727

https://pmi.spmi.ru/pmi/article/view/16727

Геология

Geology

Pegmatites of the Larsemann Hills oasis, East Antarctica: new field geological and geophysical data

Пегматиты оазиса Холмы Ларсеманн, Восточная Антарктида: новые полевые геологические и геофизические данные

Babenko

Ivan A.

Бабенко

И. А.

Babenko

Ivan A.

babenko_ivan@vk.com

0009-0000-5282-3883

Санкт-Петербургский горный университет императрицы Екатерины II (Санкт-Петербург, Россия) Empress Catherine II Saint Petersburg Mining University (Saint Petersburg, Russia)

Talovina

Irina V.

Таловина

И. В.

Talovina

Irina V.

i.talovina@gmail.com

0000-0003-4132-7010

Ushakov

Dmitrii E.

Ушаков

Д. Е.

Ushakov

Dmitrii E.

ushakov_de@pers.spmi.ru

0009-0009-6882-3955

Krikun

Nikita S.

Крикун

Н. С.

Krikun

Nikita S.

nsKrikun@gmail.com

0000-0003-0350-4987

07 07 2025

2025

273 65 79 17 04 2025 05 06 2025 07 07 2025

2025

И. А. Бабенко, И. В. Таловина, Д. Е. Ушаков, Н. С. Крикун

Ivan A. Babenko, Irina V. Talovina, Dmitrii E. Ushakov, Nikita S. Krikun

CC BY 4.0

https://pmi.spmi.ru/pmi/article/view/16727

Приводятся новые данные о различных типах пегматитов оазиса Холмы Ларсеманн (Земля Принцессы Елизаветы, Восточная Антарктида), собранные в ходе сезонных полевых работ 70-й Российской антарктической экспедиции в 2024-2025 гг. В результате комплексных геолого-геофизических исследований были описаны, проанализированы и впервые систематизированы в едином контексте все пегматитовые образования данной территории, относящиеся к различным стадиям Пан-Африканского орогенеза. Наряду с ранее известными пегматитами, связанными с деформационными этапами D2-3, D4 и post-D4, предложено их дополнительное разделение на основе минерально-геохимических признаков и по содержанию естественных радионуклидов на боросиликатные D2-3, редкометалльные D4, мусковитовые post-D4, а также выделение двух дополнительных типов, ранее не описанных в данном регионе – калишпатовых D4' и камерных редкометалльных пегматитов post-D4', отличающихся по морфологии, минералогии и геохимическим характеристикам. Особое внимание уделено структурно-тектоническому контролю пегматитовых тел, их геологическому положению, изучению зональности, а также результатам гамма-спектрометрической и магнитной съемки. Изучены пегматитовые образования, содержащие редкие типоморфные минералы – турмалин, боралсилит, грандидьерит и хризоберилл. Результаты исследований указывают на значительное разнообразие условий формирования данных пегматитов, позволяют уточнить термобарические характеристики и возраст начальных и финальных стадий Пан-Африканского метаморфического события, а также подтвердить генетическую связь пегматитовых образований с деформационными событиями D2-D4 и реконструировать этапы раннепалозойского пегматитообразования в ходе анатектических процессов в контексте геодинамической эволюции Восточной Антарктиды и Гондваны.

This paper presents new data on various types of pegmatites from the Larsemann Hills oasis (Princess Elizabeth Land, East Antarctica), collected during the 70th Russian Antarctic Expedition in 2024-2025. As a result of comprehensive geological and geophysical investigations, all pegmatite occurrences in the area belonging to different stages of the Pan-African orogeny have been described, analyzed, and systematically classified in a unified context for the first time. In addition to previously known pegmatites associated with deformation stages D2-3, D4, and post-D4, a further subdivision is proposed based on mineralogical-geochemical characteristics and the content of natural radionuclides. These include borosilicate D2-3 pegmatites, rare-metal D4 pegmatites, muscovite-bearing post-D4 pegmatites, as well as two newly identified types not previously described in the region: K-feldspar D4' pegmatites and miarolitic rare-metal post-D4' pegmatites, which differ in morphology, mineralogy, and geochemical features. Special attention is given to the structural-tectonic control of pegmatite bodies, their geological setting, zoning patterns, and the results of gamma spectrometric and magnetic surveys. Pegmatitic formations containing rare typomorphic minerals – such as tourmaline, boralsilite, grandidierite, and chrysoberyl – are also examined. The results indicate a significant diversity of pegmatite formation conditions, help refine the PT parameters and timing of the initial and final stages of the Pan-African metamorphic event, and confirm the genetic link between pegmatite development and D2-D4 deformation stages. These findings contribute to the reconstruction of Early Paleozoic pegmatite-forming stages during anatectic processes in the geodynamic evolution of East Antarctica and Gondwana.

Ключевые слова пегматиты Восточная Антарктида оазис Холмы Ларсеманн станция Прогресс Пан-Африканский орогенез редкометалльная минерализация боросиликаты гамма-спектрометрия

Keywords pegmatites East Antarctica Larsemann Hills oasis Progress Station Pan-African orogeny rare-metal mineralization borosilicates gamma spectrometry

Исследования проводятся с помощью субсидии на выполнение Государственного задания в сфере научной деятельности на 2024 г. (№ FSRW-2024-0003).

This research was carried out with support from the State assignment grant for scientific research in 2024 (N FSRW-2024-0003).

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