ЭВОЛЮЦИЯ ЭСТОНСКОГО ДОКЕМБРИЙСКОГО КРИСТАЛЛИЧЕСКОГО ФУНДАМЕНТА: ГЕОЛОГИЧЕСКИЕ, ГЕОФИЗИЧЕСКИЕ И ГЕОХРОНОЛОГИЧЕСКИЕ ОГРАНИЧЕНИЯ
Аннотация
гравитационного и магнитного полей). Кристаллический фундамент Эстонии делится на две крупные геологические единицы – Северо-Эстонский амфиболитовый и Южно-Эстонский гранулитовый комплексы. Дальнейшее деление включает шесть структурно-петрологических зон, таких как Таллиннская, Алутагузе, Йыхви,Западно-Эстонская, Тапа и Южно-Эстонская. В данной статье представлен обнов-
ленный обзор докембрийского фундамента Эстонии, типов слагающих его горных пород, геофизических полей, геохронологии, метаморфизма и металлогенеза.
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DOI: http://dx.doi.org/10.17076/geo1185
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