A three-dimensional geophysical model of the Earth’s crust in the central part of the Karelian Craton

The study of the deep structure and evolution of the Early Precambrian crust of the Earth is related to the priority problems of modern geological studies. For a number of years, geological and geophysical investigations of the Fennoscandian Shield have been carried out within multilateral internati...

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Bibliographic Details
Published in:Doklady earth sciences 2015-08, Vol.463 (2), p.808-812
Main Authors: Pashkevich, I. K., Savchenko, A. S., Starostenko, V. I., Sharov, N. V.
Format: Article
Language:English
Subjects:
Analysis
Cratons
Crust
Earth
Earth and Environmental Science
Earth Sciences
Geological time
Geology
Geophysics
International cooperation
Precambrian
Seismology
Studies
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Summary:The study of the deep structure and evolution of the Early Precambrian crust of the Earth is related to the priority problems of modern geological studies. For a number of years, geological and geophysical investigations of the Fennoscandian Shield have been carried out within multilateral international cooperation, which includes a wide range of works using the meth ods of seismology, geoelectricity, gravimetric, magne tometric, and geothermal observations. Multidisci plinary analysis of the geological and deep geophysical information has allowed us to address the existing models and develop the new models of the deep struc ture and evolution of the Early Precambrian crust of the shield.
ISSN:1028-334X
1531-8354
DOI:10.1134/S1028334X1508005X