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

XGNKDQ

pmi-16214

https://pmi.spmi.ru/pmi/article/view/16214

Геология

Geology

Mineral composition and thermobarometry of metamorphic rocks of Western Ny Friesland, Svalbard

Минеральный состав и термобарометрия метаморфических пород Западного Ню-Фрисланда, Шпицберген

Gulbin

Yurii L.

Гульбин

Ю. Л.

Gulbin

Yurii L.

ygulbin@yandex.ru

0000-0003-3631-6843

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

Akbarpuran Khaiyati

Sima A.

Акбарпуран Хайяти

С. А.

Akbarpuran Khaiyati

Sima A.

Akbarpuran_KhS@pers.spmi.ru

0000-0002-6089-9658

Sirotkin

Aleksandr N.

Сироткин

А. Н.

Sirotkin

Aleksandr N.

pechenga-67@yandex.ru

0000-0003-2433-3953

ВНИИОкеангеология им. И.С.Грамберга (Санкт-Петербург, Россия) Russian Research Institute for Geology and Mineral Resources of the World Ocean named after I.S.Gramberg (Saint Petersburg, Russia)

27 10 2023

2023

263 657 673 30 03 2023 21 09 2023 27 10 2023

2023

Ю. Л. Гульбин, С. А. Акбарпуран Хайяти, А. Н. Сироткин

Yurii L. Gulbin, Sima A. Akbarpuran Khaiyati, Aleksandr N. Sirotkin

Эта статья доступна по лицензии Creative Commons Attribution 4.0 International (CC BY 4.0)

This article is licensed under a Creative Commons Attribution 4.0 International License (CC BY 4.0)

https://pmi.spmi.ru/pmi/article/view/16214

Представлены результаты изучения минерального состава и микроструктурных особенностей представительных образцов метапелитовых и известковых сланцев, а также амфибол-биотитовых гнейсов, залегающих в северной части антиклинория Западного Ню-Фрисланда. Состав минералов был проанализирован методом SEM-EDS (JSM-6510LA с энергодисперсионным спектрометром JED-2200). На основе комплекса минеральных геотермометров (гранат-биотитового, «Ti-в-биотите», «Ti-в-мусковите», «Ti-в-амфиболе», гранат-амфиболового, амфибол-плагиоклазового, хлоритового) и геотермобарометров (GASP, GBPQ, GRIPS, GBPQ, фенгитового и др.) оценены условия метаморфизма и показано, что в породах палеопротерозойской серии Атомфьелла, слагающих западное крыло антиклинория, пиковая температура и давление соответствовали высокобарической части верхней амфиболитовой фации (690-720 °С, 9-12 кбар), в породах серии Моссель, развитых в восточном крыле и перекрывающих отложения серии Атомфьелла, – высокобарической части нижней амфиболитовой фации (580-600 °С, 9-11 кбар). Наряду с высокотемпературными парагенезисами Ms-Bt-Grt-Pl (±Ky, St), Bt-Grt-Pl-Kfs-Cal (±Scp), Bt-Hbl-Ep-Grt-Pl в породах обеих серий развита низкотемпературная ассоциация Ms-Chl-Ep-Ab-Prh-Ttn, образовавшаяся в условиях перехода от зеленосланцевой к пренит-пумпеллиитовой фации (260-370 °С).

The results of the study of mineral composition and microstructure of representative metapelitic and calcic pelitic schist and amphibole-biotite gneiss, occurring in the northern part of the Western Ny Friesland anticlinorium, are reported. Mineral composition was analyzed with a JSM-6510LA scanning electron microscope with a JED-2200 (JEOL) energy dispersive spectrometer. Metamorphic conditions were assessed with various mineral geothermometers (garnet-biotite, Ti-in-biotite, Ti-in-muscovite, Ti-in-amphibole, garnet-amphibole, amphibole-plagioclase, and chlorite) and geothermobarometers (GASP, GBPQ, GRIPS, GBPQ, phengite, etc.). It has been shown that peak temperature and pressure for rocks of the Paleoproterozoic Atomfjella Series forming the western limb of the anticlinorium are consistent with those for the high-pressure part of the upper amphibolite facies (690-720 °С, 9-12 kbar), and the peak temperature and pressure for rocks of the Mossel Series occurring in the eastern limb and rest on the Atomfjella rock sequence, are consistent with the high-pressure part of the lower amphibolite facies (580-600 °С, 9-11 kbar). In addition to the high-temperature parageneses Ms-Bt-Grt-Pl (±Ky, St), Bt-Grt-Pl-Kfs-Cal (±Scp) and Bt-Hbl-Ep-Grt-Pl, the rocks of the both series display the low-temperature assemblage Ms-Chl-Ep-Ab-Prh-Ttn, which was formed upon transition from greenschist to prehnite-pumpellyite facies (260-370 °С).

Ключевые слова метапелитовые и известковые сланцы амфибол-биотитовый гнейс минеральная термобарометрия условия метаморфизма Ню-Фрисланд Шпицберген

Keywords metapelitic and calcic pelitic schist amphibole-biotite gneiss mineral thermobarometry conditions of metamorphism Ny Friesland Svalbard

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