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 CMIJJB pmi-16472 https://pmi.spmi.ru/pmi/article/view/16472 Геология Geology Mineralogy and thermobarometry of the Kalevian volcano-plutonic complex of the Kaskama block (Inari Terrane, Kola-Norwegian Region, Fennoscandian Shield) Минералогия и термобарометрия пород вулкано-плутонического комплекса калевия Каскамского блока террейна Инари (Кольско-Норвежская область Фенноскандинавского щита) Vrevsky Aleksandr B. Вревский А. Б. Vrevsky Aleksandr B. avrevsky@mail.ru 0000-0002-7038-0841 Институт геологии и геохронологии докембрия РАН (Санкт-Петербург, Россия) Institute of Precambrian Geology and Geochronology RAS (Saint Petersburg, Russia) Yurchenko Anastasiya V. Юрченко А. В. Yurchenko Anastasiya V. yurchenko-nastya@yandex.ru 0000-0002-3999-5151 Институт геологии и геохронологии докембрия РАН (Санкт-Петербург, Россия) Institute of Precambrian Geology and Geochronology RAS (Saint Petersburg, Russia) Baltybaev Shauket K. Балтыбаев Ш. К. Baltybaev Shauket K. s.k.baltybaev@ipgg.ru 0000-0002-6484-2042 Институт геологии и геохронологии докембрия РАН (Санкт-Петербург, Россия) Institute of Precambrian Geology and Geochronology RAS (Saint Petersburg, Russia) 29 04 2025 2025 274 21 34 02 05 2024 07 11 2024 25 08 2025 © 2025 А. Б. Вревский, А. В. Юрченко, Ш. К. Балтыбаев © 2025 Aleksandr B. Vrevsky, Anastasiya V. Yurchenko, Shauket K. Baltybaev 2025 А. Б. Вревский, А. В. Юрченко, Ш. К. Балтыбаев Aleksandr B. Vrevsky, Anastasiya V. Yurchenko, Shauket K. Baltybaev 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/16472

Изучены условия петрогенезиса и эволюции пород при региональном метаморфизме вулкано-плутонического комплекса каскамской структуры в пределах террейна Инари на северо-западе России. Применен детальный петрографический анализ пород, рассмотрены особенности химического состава минералов, выполнено моделирование магматического и метаморфического минералообразования. РТ-условия образования пород, наряду с ранее известными фактами, включая изотопно-геохронологические, не позволяют соотнести изученные толщи с породами беломорского комплекса, как считалось прежде. Моделирование магматического и метаморфического минералообразования показало хорошую сходимость модельных полей устойчивости минеральных парагенезисов и количественного соотношения минералов с наблюдаемыми в реальных образцах. Ранние минеральные парагенезисы магматического этапа отвечают кристаллизации ряда породообразующих и акцессорных минералов из коматиитового расплава, на них накладываются минеральные парагенезисы прогрессивного и регрессивного метаморфизма. Реликтовые магматические минералы (оливин, клинопироксен, ортопироксен, магнетит-шпинель) в метаперидотитах позволяют оценить их ликвидусные температуры в диапазоне 1480-950 °С. Прогрессивная стадия метаморфических преобразований характеризуется развитием минеральных парагенезисов: гранат + амфибол + плагиоклаз + кварц ± биотит, амфибол + плагиоклаз + кварц. Поздняя низкотемпературная регрессивная стадия метаморфизма характеризуется развитием эпидот-, цоизит-, актинолитсодержащих ассоциаций и ряда других низкотемпературных минералов. Пиковые значения параметров прогрессивного метаморфизма оцениваются как Т = 600-700 °С, Р = 5-9 кбар, для регрессивной стадии Т = 400-500 °С, Р = 3-5 кбар. Выявленные термодинамические условия эндогенного породообразования в каскамской структуре необходимо учитывать при определении принадлежности изученных вулканогенно-плутонических и метаосадочных комплексов к палеопротерозойским террейнам Кольско-Норвежской области Фенноскандинавского щита.

The petrogenesis and evolution of metamorphic rocks of the volcano-plutonic units of the Kaskama block of the Inari Terrane in northwestern Russia were studied. A petrographic and mineral study and modeling of igneous and metamorphic mineral formation were performed. PT-conditions of rocks, along with previously known data, including geochronological ones, do not allow us to correlate the studied units with rocks of the Belomorian complex, as previously thought. Modeling of igneous and metamorphic mineral shows good convergence with the fields of stability of mineral parageneses and quantitive ratio of minerals with those observed in the real samples. The early mineral parageneses of the magmatic stage corresponds to the crystallization of rock-forming and accessory minerals from the komatiite melt, and mineral parageneses of progressive and regressive metamorphism stages are superimposed on them. Relic igneous minerals (olivine, clinopyroxene, orthopyroxene, magnetite-spinel) in metaperidotites make it possible to estimate their liquidus temperatures in the range of 1,480-950 °С. The progressive stage of metamorphism is characterized by the development of mineral parageneses: garnet + amphibole + plagioclase + quartz ± biotite, amphibole + plagioclase + quartz. The late low-temperature regressive stage of metamorphism is characterized by the development of epidote-, zoisite-, actinolite-containing associations and a number of other low-temperature minerals. Peak parameters of progressive metamorphism are estimated as Т = 600-700 °С, Р = 5-9 kbar and for the regressive stage as Т = 400-500 °С, Р = 3-5 kbar. The identified thermodynamic conditions for the Kaskama block should be considered when determining whether the studied volcano-plutonic and metasedimentary units belong to the Paleoproterozoic terranes of the Kola-Norwegian Region of the Fennoscandian Shield.

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