THE EVOLUTION OF THE ESTONIAN PRECAMBRIAN BASEMENT: GEOLOGICAL, GEOPHYSICAL AND GEOCHRONOLOGICAL CONSTRAINTS

The Estonian Precambrian crystalline basement that consists of Paleo- to Meso-Proterozoic metamorphic and igneous rocks is covered by a 100-780 m thick deposit of Paleozoic sedimentary rocks. Thus, the basement is unavailable for direct surficial observations and our present knowledge is based on in...

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Bibliographic Details
Main Authors: Алвар Соэсоо, Сиим Нирги, Юри Пладо, Alvar Soesoo, Siim Nirgi, Jüri Plado
Format: Article
Language:English
Published: Karelian Research Centre of the Russian Academy of Sciences 2020-02-01
Series:Transactions of the Karelian Research Centre of the Russian Academy of Sciences
Subjects:
Online Access:http://journals.krc.karelia.ru/index.php/precambrian/article/view/1185